首页 > 最新文献

Geologica Acta最新文献

英文 中文
Post-rift extensional tectonics at the edge of a carbonate platform: insights from the Middle Jurassic-Early Cretaceous Monte Giano stratigraphic record (central Apennines, Italy) 碳酸盐岩平台边缘的裂谷后伸展构造:来自中侏罗世-早白垩世Monte Giano地层记录的见解(意大利亚平宁中部)
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-10-15 DOI: 10.1344/geologicaacta2021.19.12
F. Capotorti, C. Muraro
A new interpretation of the Middle Jurassic-Early Cretaceous paleogeographic evolution of the NW sector of the Latium-Abruzzi carbonate platform facing the Umbria-Marche Basin is proposed, based on Monte Giano area (central Apennines, Italy). During Late Triassic-early Bajocian time, the area was characterized by shallow water sedimentation. Inner and marginal carbonate platform deposits are overlain by pelagic deposits (Posidonia level), early Bajocian p.p. in age. This unconformity testifying the sudden drowning of the Monte Giano area, while shallow water sedimentation persisted in the remaining sectors of the carbonate platform. The Posidonia level is paraconformably overlain by distal slope deposits of the Velino Gorge limestones Formation, Kimmeridgian p.p.-Tithonian p.p. in age. Therefore, a 12Ma gap is recorded as in the Umbria-Marche Basin pelagic carbonate platforms. An extensional Bajocian tectonic phase, possibly related to the Piemont-Ligurian Ocean opening coupled with rheologic differences at the basin/platform boundary, drastically changed the regional paleogeography causing the breakup and the drowning of the NW sector of the Latium-Abruzzi carbonate platform and the creation of a large flat-topped pelagic carbonate platform. The estimate offset of the early Bajocian fault is around 300-350m. The Velino Gorge limestones fm. pass laterally and vertically to the Upper Tithonian platform-margin reef complex of the Ellipsactinia limestones fm.; these units constitute a shallowing and coarsening upward sequence and levelled the paleobathymetric gradient created by the Bajocian extension. The progradation of the Latium-Abruzzi carbonate platform continued during Early Cretaceous time. These results have strong implications on the tectonic and paleogeographic evolution of the major domains of the central Apennines.
基于Monte Giano地区(意大利亚平宁山脉中部),提出了面向Umbria-Marche盆地的Latium-Abruzzi碳酸盐岩台地NW段中侏罗世-早白垩世古地理演化的新解释。晚三叠世—早巴约修期,该区以浅水沉积为主。内、边缘碳酸盐岩台地沉积上覆有早巴约修期的上层沉积(波西多尼亚水平)。这种不整合证明了Monte Giano地区的突然淹没,而碳酸盐岩台地的其余部分则持续存在浅水沉积。波西多尼亚水平上覆有基默里吉纪-梯东纪的Velino峡谷灰岩组远端斜坡沉积。因此,在Umbria-Marche盆地中上层碳酸盐岩台地中记录了12Ma的缺口。一个伸展的巴约期构造阶段,可能与皮埃山-利古里亚海洋张开有关,加上盆地/台地边界的流变学差异,极大地改变了区域古地理,导致Latium-Abruzzi碳酸盐岩台地的NW段破裂和淹没,形成了一个大型平顶的上层碳酸盐岩台地。巴约谦早期断层的估计偏移量在300-350米左右。维利诺峡谷的石灰岩。横向和纵向通至上梯统台缘礁杂岩的椭圆岩系灰岩;这些单元构成了一个浅化、粗化的向上层序,平整了巴约西亚伸展所形成的古水深梯度。早白垩世,Latium-Abruzzi碳酸盐岩台地继续沉积。这些结果对亚平宁山脉中部主要构造域的构造和古地理演化具有重要意义。
{"title":"Post-rift extensional tectonics at the edge of a carbonate platform: insights from the Middle Jurassic-Early Cretaceous Monte Giano stratigraphic record (central Apennines, Italy)","authors":"F. Capotorti, C. Muraro","doi":"10.1344/geologicaacta2021.19.12","DOIUrl":"https://doi.org/10.1344/geologicaacta2021.19.12","url":null,"abstract":"A new interpretation of the Middle Jurassic-Early Cretaceous paleogeographic evolution of the NW sector of the Latium-Abruzzi carbonate platform facing the Umbria-Marche Basin is proposed, based on Monte Giano area (central Apennines, Italy). During Late Triassic-early Bajocian time, the area was characterized by shallow water sedimentation. Inner and marginal carbonate platform deposits are overlain by pelagic deposits (Posidonia level), early Bajocian p.p. in age. This unconformity testifying the sudden drowning of the Monte Giano area, while shallow water sedimentation persisted in the remaining sectors of the carbonate platform. The Posidonia level is paraconformably overlain by distal slope deposits of the Velino Gorge limestones Formation, Kimmeridgian p.p.-Tithonian p.p. in age. Therefore, a 12Ma gap is recorded as in the Umbria-Marche Basin pelagic carbonate platforms. An extensional Bajocian tectonic phase, possibly related to the Piemont-Ligurian Ocean opening coupled with rheologic differences at the basin/platform boundary, drastically changed the regional paleogeography causing the breakup and the drowning of the NW sector of the Latium-Abruzzi carbonate platform and the creation of a large flat-topped pelagic carbonate platform. The estimate offset of the early Bajocian fault is around 300-350m. The Velino Gorge limestones fm. pass laterally and vertically to the Upper Tithonian platform-margin reef complex of the Ellipsactinia limestones fm.; these units constitute a shallowing and coarsening upward sequence and levelled the paleobathymetric gradient created by the Bajocian extension. The progradation of the Latium-Abruzzi carbonate platform continued during Early Cretaceous time. These results have strong implications on the tectonic and paleogeographic evolution of the major domains of the central Apennines.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45653379","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Crandallite-rich beds of the Libkovice Member, Most Basin, Czech Republic: climatic extremes or paleogeographic changes at the onset of the Miocene Climatic Optimum? 捷克共和国大多数盆地Libkovice成员富长晶石层:中新世气候最佳期开始时的极端气候或古地理变化?
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-09-20 DOI: 10.1344/geologicaacta2021.19.11
K. Mach, V. Rapprich, M. Faměra, M. Havelcová, T. Matys Grygar, T. Novotný, M. Rehor, Yulia V. Erban Kochergina
We describe the occurrence and possible origin of rare beds 1–10cm thick and containing 20–70% of crandallite, a Ca-Al phosphate enriched in Sr and Ba, found within otherwise monotonous clay-rich lacustrine sediments of the Most Basin in the Central-European Neogene Ohře Rift system. The beds were formed at ca. 17.31, 17.06, and 16.88Ma, while the entire suite of monotonous clays of the Libkovice Member was deposited between 17.46 and 16.65Ma. Trace-element and organic geochemistry, Ar-Ar geochronology and C-O-Sr isotope systematics are used to infer their source and processes leading to their formation. The most enigmatic aspect of the formation of the crandallite beds is the removal of a huge amount of phosphorus from its biogenic cycle in the lacustrine system, which was otherwise stable for ca. 0.8My. Formation of detritus-poor crandallite beds could result from some exceptional environmental disruptions that hindered transport of fine clastic material to the basin floor. Silicic volcanic activity in the area of the Pannonian Basin could have triggered this disruption. Crandallite could provide evidence of long-lasting droughts and acidification of the exogenic environment, as they are roughly coeval with the onset of the Miocene Climatic Optimum at ca. 17.0Ma.
我们描述了厚度为1–10cm、含有20–70%裂隙岩(一种富含Sr和Ba的Ca-Al磷酸盐)的稀有矿层的出现和可能的起源,该矿床位于中欧新第三纪奥热裂谷系Most盆地的单调富含粘土的湖泊沉积物中。矿层形成于约17.31、17.06和16.88Ma,而Libkovice段的整套单调粘土沉积于17.46和16.65Ma之间。微量元素和有机地球化学、Ar-Ar地质年代学和C-O-Sr同位素系统学用于推断其来源和形成过程。裂隙岩床形成最神秘的方面是从湖泊系统中的生物循环中去除了大量的磷,否则湖泊系统在约0.8My内是稳定的。缺乏碎屑的裂隙岩床的形成可能是由于一些特殊的环境破坏,阻碍了细碎屑物质向盆地底部的运输。潘诺尼亚盆地地区的硅质火山活动可能引发了这种破坏。Crandallite可以提供长期干旱和外部环境酸化的证据,因为它们与约17.0Ma的中新世气候最佳期大致同期。
{"title":"Crandallite-rich beds of the Libkovice Member, Most Basin, Czech Republic: climatic extremes or paleogeographic changes at the onset of the Miocene Climatic Optimum?","authors":"K. Mach, V. Rapprich, M. Faměra, M. Havelcová, T. Matys Grygar, T. Novotný, M. Rehor, Yulia V. Erban Kochergina","doi":"10.1344/geologicaacta2021.19.11","DOIUrl":"https://doi.org/10.1344/geologicaacta2021.19.11","url":null,"abstract":"We describe the occurrence and possible origin of rare beds 1–10cm thick and containing 20–70% of crandallite, a Ca-Al phosphate enriched in Sr and Ba, found within otherwise monotonous clay-rich lacustrine sediments of the Most Basin in the Central-European Neogene Ohře Rift system. The beds were formed at ca. 17.31, 17.06, and 16.88Ma, while the entire suite of monotonous clays of the Libkovice Member was deposited between 17.46 and 16.65Ma. Trace-element and organic geochemistry, Ar-Ar geochronology and C-O-Sr isotope systematics are used to infer their source and processes leading to their formation. The most enigmatic aspect of the formation of the crandallite beds is the removal of a huge amount of phosphorus from its biogenic cycle in the lacustrine system, which was otherwise stable for ca. 0.8My. Formation of detritus-poor crandallite beds could result from some exceptional environmental disruptions that hindered transport of fine clastic material to the basin floor. Silicic volcanic activity in the area of the Pannonian Basin could have triggered this disruption. Crandallite could provide evidence of long-lasting droughts and acidification of the exogenic environment, as they are roughly coeval with the onset of the Miocene Climatic Optimum at ca. 17.0Ma.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42686060","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Critical analysis of Mediterranean sea level limit cycles during the Messinian salinity crisis 墨西尼亚盐度危机期间地中海海平面极限旋回的关键分析
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-08-24 DOI: 10.1344/GeologicaActa2021.19.10
M. Baum
The Messinian Salinity Crisis (5.97-5.33Ma) may be one of the most significant periods of sea-level change in recent geologic history. During this period, evaporite deposition throughout the Mediterranean basin records a series of dramatic environmental changes as flow through the Strait of Gibraltar was restricted. In the first stage of evaporite deposition, cycles of gypsum appear in shallow basins on the margins of the Mediterranean. The complex environmental history giving rise to these cycles has been investigated for decades but remains controversial. Notably, whether the evaporites are connected to significant changes in Mediterranean sea level is an open question.In one proposed model, competition between tectonic uplift and erosion at the Strait of Gibraltar gives rise to selfsustaining sea-level oscillations—limit cycles—which trigger evaporite deposition. Here I show that limit cycles are not a robust result of the proposed model and discuss how any oscillations produced by this model depend on an unrealistic formulation of a key model equation. First, I simplify the model equations and test whether limit cycles are produced in 64 million unique combinations of model parameters, finding oscillations in only 0.2% of all simulations. Next, I examine the formulation of a critical model equation representing stream channel slope over the Strait of Gibraltar, concluding that a more realistic formulation would render sea-level limit cycles improbable, if not impossible, in the proposed model.
墨西尼亚盐度危机(5.97-5.33Ma)可能是近代地质史上海平面变化最显著的时期之一。在此期间,由于流经直布罗陀海峡的水流受到限制,整个地中海盆地的蒸发岩沉积记录了一系列剧烈的环境变化。在蒸发岩沉积的第一阶段,地中海边缘的浅盆地中出现了石膏旋回。导致这些周期的复杂环境历史已经被研究了几十年,但仍然存在争议。值得注意的是,蒸发岩是否与地中海海平面的显著变化有关是一个悬而未决的问题。在一个提出的模型中,直布罗陀海峡的构造抬升和侵蚀之间的竞争导致了自维持的海平面振荡——极限循环——从而触发蒸发岩沉积。在这里,我证明了极限环不是所提出模型的稳健结果,并讨论了该模型产生的任何振荡如何取决于关键模型方程的不切实际的公式。首先,我简化了模型方程,并测试了6400万个独特的模型参数组合是否产生了极限环,仅在0.2%的模拟中发现了振荡。接下来,我研究了代表直布罗陀海峡河道坡度的临界模型方程的公式,得出的结论是,更现实的公式将使拟议模型中的海平面极限周期即使不是不可能,也不可能。
{"title":"Critical analysis of Mediterranean sea level limit cycles during the Messinian salinity crisis","authors":"M. Baum","doi":"10.1344/GeologicaActa2021.19.10","DOIUrl":"https://doi.org/10.1344/GeologicaActa2021.19.10","url":null,"abstract":"The Messinian Salinity Crisis (5.97-5.33Ma) may be one of the most significant periods of sea-level change in recent geologic history. During this period, evaporite deposition throughout the Mediterranean basin records a series of dramatic environmental changes as flow through the Strait of Gibraltar was restricted. In the first stage of evaporite deposition, cycles of gypsum appear in shallow basins on the margins of the Mediterranean. The complex environmental history giving rise to these cycles has been investigated for decades but remains controversial. Notably, whether the evaporites are connected to significant changes in Mediterranean sea level is an open question.\u0000In one proposed model, competition between tectonic uplift and erosion at the Strait of Gibraltar gives rise to selfsustaining sea-level oscillations—limit cycles—which trigger evaporite deposition. Here I show that limit cycles are not a robust result of the proposed model and discuss how any oscillations produced by this model depend on an unrealistic formulation of a key model equation. First, I simplify the model equations and test whether limit cycles are produced in 64 million unique combinations of model parameters, finding oscillations in only 0.2% of all simulations. Next, I examine the formulation of a critical model equation representing stream channel slope over the Strait of Gibraltar, concluding that a more realistic formulation would render sea-level limit cycles improbable, if not impossible, in the proposed model.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-08-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45061132","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geochemistry of Granitoids in Central Sumatra: An Identification of Plate Extension during Triassic 苏门答腊中部花岗岩类地球化学:三叠纪板块伸展的识别
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-07-26 DOI: 10.1344/geologicaacta2021.19.9
Ronaldo Irzon, I. Syafri, N. Suwarna, J. Hutabarat, P. Sendjaja, V. E. Setiawan
Previous investigations of granitoids in Sumatra were focused on age dating with minimum geochemistry composition analysis. The purpose of this study is to define the geochemistry classification of the intrusions in central Sumatra and to explain the rocks' correlation to Southeast Asia tectonic activities. A polarizing microscope was used for petrography description while XRF and ICP-MS were applied for geochemistry measurements. According to the geochemistry, almost all of the intrusions are the I-type volcanic arc granitoids. The oldest studied rock is the Late Permian Ombilin Granite that should have been formed before West Sumatra and West Burma move away from the Cathaysia. Sulit Air Granite and Tanjung Gadang Granite intrusion were triggered by the subduction of Meso-Tethys beneath West Sumatra while Lassi Pluton and Lolo Pluton due to Indo-Australia and West Sumatra convergency. The Triassic Sijunjung Granite depicts A-type granite natures to suggest an extension in the West Sumatra plate.
以往对苏门答腊花岗岩类的研究主要集中在年龄测年和最少的地球化学成分分析。本研究的目的是确定苏门答腊中部侵入岩的地球化学分类,并解释岩石与东南亚构造活动的相关性。岩石学描述采用偏光显微镜,地球化学测量采用XRF和ICP-MS。根据地球化学特征,这些侵入体几乎都是i型火山弧花岗岩类。研究中最古老的岩石是晚二叠世的Ombilin花岗岩,它应该是在西苏门答腊和西缅甸离开华夏之前形成的。Sulit Air花岗岩和Tanjung Gadang花岗岩的侵入是由中特提斯俯冲在西苏门答腊下方引发的,而Lassi和Lolo岩体则是由印-澳大利亚和西苏门答腊辐合引起的。三叠纪四军中花岗岩为a型花岗岩,显示出西苏门答腊板块的伸展。
{"title":"Geochemistry of Granitoids in Central Sumatra: An Identification of Plate Extension during Triassic","authors":"Ronaldo Irzon, I. Syafri, N. Suwarna, J. Hutabarat, P. Sendjaja, V. E. Setiawan","doi":"10.1344/geologicaacta2021.19.9","DOIUrl":"https://doi.org/10.1344/geologicaacta2021.19.9","url":null,"abstract":"Previous investigations of granitoids in Sumatra were focused on age dating with minimum geochemistry composition analysis. The purpose of this study is to define the geochemistry classification of the intrusions in central Sumatra and to explain the rocks' correlation to Southeast Asia tectonic activities. A polarizing microscope was used for petrography description while XRF and ICP-MS were applied for geochemistry measurements. According to the geochemistry, almost all of the intrusions are the I-type volcanic arc granitoids. The oldest studied rock is the Late Permian Ombilin Granite that should have been formed before West Sumatra and West Burma move away from the Cathaysia. Sulit Air Granite and Tanjung Gadang Granite intrusion were triggered by the subduction of Meso-Tethys beneath West Sumatra while Lassi Pluton and Lolo Pluton due to Indo-Australia and West Sumatra convergency. The Triassic Sijunjung Granite depicts A-type granite natures to suggest an extension in the West Sumatra plate.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66405241","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Silt-sized sediments and gypsum on surface formations in the Ebro valley. A disambiguation of the term gypsiferous silts 埃布罗河谷地表沉积物和石膏。石膏质泥沙一词的消歧义
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-06-23 DOI: 10.1344/geologicaacta2021.19.8
R. Poch, R. Rodríguez‐Ochoa, O. Artieda, J. Balasch, J. Boixadera
Since the 60’s, many authors have reported the presence of common silt-sized materials in the Ebro valley, on surface formations and positions that have given rise to several interpretations, sometimes contradictory. According to the references, three main terms are used (gypsiferous silts, loess and flour-like gypsum) applied to silts and fine sands with gypsum accumulations. The two first terms are applied to materials with carbonate contents up to 40-50%, coarse silty to fine sandy textures, and located in different positions. Loess normally appears as thick outcrops on slopes leeward from the main wind direction, with a limited pedogenesis consisting of a partial carbonate mobilisation and gypsum contents between 0 and 30%. The third (gypsum-rich) type has a variable spatial distribution, appearing between limestone layers, along footslopes, outcropping as metric surface formations, or as generalized karstified subsurface accumulations. Their composition is almost 100% silt- to fine sand size lenticular gypsum. While some authors claim for an aeolian origin to all these materials, only part of them (loess) has a clear aeolian origin, while flour-like gypsum derives from on-site weathering of gyprock or by precipitation of calcium- and sulfate saturated watertables as it is reported to occur in many other arid regions; and the rest (gypsiferous silts sensu stricto) are mainly colluvial-alluvial. This distinction is necessary since they differ in their geotechnical behaviour and properties relevant for agricultural land uses, therefore they should be taken into account when carrying out geological mappings or soil surveys in this and similar arid regions.
自20世纪60年代以来,许多作者报道了埃布罗河谷中常见的泥沙大小的物质的存在,这些物质的表面构造和位置产生了几种解释,有时是相互矛盾的。根据文献资料,对含石膏堆积物的粉砂和细砂主要使用了三个术语(含石膏粉砂、黄土和粉状石膏)。前两个术语适用于碳酸盐含量高达40-50%,粗粉质到细砂质质地,并且位于不同位置的材料。黄土通常以厚露头出现在主风向背风的斜坡上,其土壤成因有限,由部分碳酸盐活化和石膏含量在0 - 30%之间组成。第三种(富石膏)类型具有可变的空间分布,出现在石灰石层之间,沿着脚坡,以公制地表地层或广义岩溶地下堆积的形式露头。它们的成分几乎100%是粉砂到细砂大小的透镜状石膏。虽然有些作者声称所有这些材料都是风成成因,但其中只有一部分(黄土)有明确的风成成因,而面粉状石膏则来自于现场风化的旋盖岩或钙和硫酸盐饱和地下水位的沉淀,据报道,这在许多其他干旱地区都发生过;其余(严格意义上的石膏质粉砂)主要为集体冲积型。这种区别是必要的,因为它们在与农业土地使用有关的地质技术行为和性质上有所不同,因此在这个和类似的干旱地区进行地质测绘或土壤调查时应考虑到它们。
{"title":"Silt-sized sediments and gypsum on surface formations in the Ebro valley. A disambiguation of the term gypsiferous silts","authors":"R. Poch, R. Rodríguez‐Ochoa, O. Artieda, J. Balasch, J. Boixadera","doi":"10.1344/geologicaacta2021.19.8","DOIUrl":"https://doi.org/10.1344/geologicaacta2021.19.8","url":null,"abstract":"Since the 60’s, many authors have reported the presence of common silt-sized materials in the Ebro valley, on surface formations and positions that have given rise to several interpretations, sometimes contradictory. According to the references, three main terms are used (gypsiferous silts, loess and flour-like gypsum) applied to silts and fine sands with gypsum accumulations. The two first terms are applied to materials with carbonate contents up to 40-50%, coarse silty to fine sandy textures, and located in different positions. Loess normally appears as thick outcrops on slopes leeward from the main wind direction, with a limited pedogenesis consisting of a partial carbonate mobilisation and gypsum contents between 0 and 30%. The third (gypsum-rich) type has a variable spatial distribution, appearing between limestone layers, along footslopes, outcropping as metric surface formations, or as generalized karstified subsurface accumulations. Their composition is almost 100% silt- to fine sand size lenticular gypsum. While some authors claim for an aeolian origin to all these materials, only part of them (loess) has a clear aeolian origin, while flour-like gypsum derives from on-site weathering of gyprock or by precipitation of calcium- and sulfate saturated watertables as it is reported to occur in many other arid regions; and the rest (gypsiferous silts sensu stricto) are mainly colluvial-alluvial. This distinction is necessary since they differ in their geotechnical behaviour and properties relevant for agricultural land uses, therefore they should be taken into account when carrying out geological mappings or soil surveys in this and similar arid regions.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-06-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46286085","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Late Quaternary subsidence records from the Datça graben and Cnidus ancient city (SW Turkey): sea-level changes versus tectonics 土耳其西南部datalada地堑和Cnidus古城晚第四纪沉降记录:海平面变化与构造
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-06-07 DOI: 10.1344/GEOLOGICAACTA2021.19.6
E. Özsayın, S. Üner, Burcu Kahraman
The Datca graben in southwestern Anatolia is a WNW-trending seismically active depression, with tectonic activity since Pliocene time. This tectonic activity is controlled by normal faults, which have effected ancient settlements. The Cnidus city (old and modern) –an ancient mercantile centre during the Hellenistic, Roman and Byzantine periods– is one of the places that has recorded this activity. The ancient harbour walls of Cnidus, lying 2.2-4.0m below sea level, contain important traces about sea-level changes and tectonics over the past 2.6kyr. Palaeostress analysis along boundary faults in the Datca graben yields an almost N–S oriented pure tensional regime, compatible with earthquake focal mechanism solutions located around the Datca Peninsula. Additionally, an almost E−W trending surface rupture related to a historical earthquake in modern Cnidus, which shows normal fault characteristics, gives further support to the ongoing extension along the Kizlan, Karakoy and Cnidus fault zones. Previous studies on late Quaternary sea-level changes around the Datca Peninsula suggest that 2.6kyr ago sea level was 1.0-1.25m lower than today. From the present-day depth of the Old Cnidus harbour remains and regional sea-level records, it can be inferred that tectonics has played a significant role. Our calculations show that the Datca graben is subsiding at rates of 0.36-0.46mm/yr in the central part and 1.05-1.15mm/yr in the southern part. These values match those found in other areas around the Datca Peninsula.
安纳托利亚西南部的Datca地堑是一个WNW走向的地震活动凹陷,自上新世以来就有构造活动。这种构造活动受到正断层的控制,正断层影响了古代的定居点。Cnidus城(古老和现代)是希腊化、罗马和拜占庭时期的古代商业中心,也是记录这一活动的地方之一。Cnidus的古港壁位于海平面以下2.2-4.0米处,包含了过去2.6公里海平面变化和构造的重要痕迹。沿着Datca地堑边界断层的古应力分析产生了几乎南北向的纯张性状态,与Datca半岛周围的地震震源机制解决方案相兼容。此外,与现代Cnidus的历史地震有关的几乎呈E-W走向的地表破裂,显示出正常的断层特征,为沿着Kizlan、Karakoy和Cnidus断层带的持续延伸提供了进一步的支持。先前对达特卡半岛晚第四纪海平面变化的研究表明,2.6公里前的海平面比今天低1.0-1.25米。从老Cnidus港遗迹的现今深度和区域海平面记录可以推断,构造运动发挥了重要作用。我们的计算表明,Datca地堑在中部以0.36-0.46mm/yr的速度沉降,在南部以1.05-1.15mm/yr的速率沉降。这些值与Datca半岛周围其他地区的值相匹配。
{"title":"Late Quaternary subsidence records from the Datça graben and Cnidus ancient city (SW Turkey): sea-level changes versus tectonics","authors":"E. Özsayın, S. Üner, Burcu Kahraman","doi":"10.1344/GEOLOGICAACTA2021.19.6","DOIUrl":"https://doi.org/10.1344/GEOLOGICAACTA2021.19.6","url":null,"abstract":"The Datca graben in southwestern Anatolia is a WNW-trending seismically active depression, with tectonic activity since Pliocene time. This tectonic activity is controlled by normal faults, which have effected ancient settlements. The Cnidus city (old and modern) –an ancient mercantile centre during the Hellenistic, Roman and Byzantine periods– is one of the places that has recorded this activity. The ancient harbour walls of Cnidus, lying 2.2-4.0m below sea level, contain important traces about sea-level changes and tectonics over the past 2.6kyr. Palaeostress analysis along boundary faults in the Datca graben yields an almost N–S oriented pure tensional regime, compatible with earthquake focal mechanism solutions located around the Datca Peninsula. Additionally, an almost E−W trending surface rupture related to a historical earthquake in modern Cnidus, which shows normal fault characteristics, gives further support to the ongoing extension along the Kizlan, Karakoy and Cnidus fault zones. Previous studies on late Quaternary sea-level changes around the Datca Peninsula suggest that 2.6kyr ago sea level was 1.0-1.25m lower than today. From the present-day depth of the Old Cnidus harbour remains and regional sea-level records, it can be inferred that tectonics has played a significant role. Our calculations show that the Datca graben is subsiding at rates of 0.36-0.46mm/yr in the central part and 1.05-1.15mm/yr in the southern part. These values match those found in other areas around the Datca Peninsula.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45608362","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
40Ar/39Ar geochronology of Burdigalian paleobotanical localities in the central Paratethys (south Slovakia) Paratethys中部(斯洛伐克南部)Burdigalian古植物区的40Ar/39Ar地质年代
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-05-21 DOI: 10.1344/GEOLOGICAACTA2021.19.5
Katarína Šarinová, S. Rybár, F. Jourdan, C. Mayers, A. Frew, M. Kováčová, Petronela Nováková, Barbara Lichtman, M. Kováč
The Lipovany and Mucin paleobotanical localities contain important floral associations within the tuff horizons, which were used for determination of subtropical to tropical climatic conditions during the Early Miocene. Based on the combination of results from plagioclase and biotite  40 Ar/ 39 Ar dating, the age of the tuff deposition is around 17.3Ma. For the Lipovany locality, single-grain  40 Ar/ 39 Ar convergent ages of 17.49±0.54Ma and 17.28±0.06Ma, for plagioclase and biotite were obtained, respectively. The Mucin locality only provide an imprecise convergent age of 16.5±1.4Ma due to the small size of the analyzed plagioclase crystals. The results thus allowed to include the fossil subtropical flora of the studied localities in the late Ottnangian regional stage (upper part of the Burdigalian). Additionally, these age data indicate that deposition of the overlaying Salgotarjan Formation starts much later than originally thought (during Ottnangian-Karpatian boundary).
Lipovany和Mucin古植物区在凝灰岩层中包含重要的植物组合,用于确定中新世早期的亚热带至热带气候条件。根据斜长石和黑云母40Ar/39Ar定年的结果,凝灰岩沉积的年龄约为17.3Ma。在Lipovany地区,斜长石和黑云母的单颗粒40Ar/39Ar会聚年龄分别为17.49±0.54Ma和17.28±0.06Ma。由于分析的斜长石晶体尺寸较小,Mucin位置仅提供16.5±1.4Ma的不精确收敛年龄。因此,研究结果包括了所研究地区在Ottnagian晚期区域阶段(Burdigalian的上部)的亚热带植物群化石。此外,这些年龄数据表明,上覆Salgotarjan组的沉积开始时间比最初认为的要晚得多(在Ottnagian-Karpatian边界期间)。
{"title":"40Ar/39Ar geochronology of Burdigalian paleobotanical localities in the central Paratethys (south Slovakia)","authors":"Katarína Šarinová, S. Rybár, F. Jourdan, C. Mayers, A. Frew, M. Kováčová, Petronela Nováková, Barbara Lichtman, M. Kováč","doi":"10.1344/GEOLOGICAACTA2021.19.5","DOIUrl":"https://doi.org/10.1344/GEOLOGICAACTA2021.19.5","url":null,"abstract":"The Lipovany and Mucin paleobotanical localities contain important floral associations within the tuff horizons, which were used for determination of subtropical to tropical climatic conditions during the Early Miocene. Based on the combination of results from plagioclase and biotite  40 Ar/ 39 Ar dating, the age of the tuff deposition is around 17.3Ma. For the Lipovany locality, single-grain  40 Ar/ 39 Ar convergent ages of 17.49±0.54Ma and 17.28±0.06Ma, for plagioclase and biotite were obtained, respectively. The Mucin locality only provide an imprecise convergent age of 16.5±1.4Ma due to the small size of the analyzed plagioclase crystals. The results thus allowed to include the fossil subtropical flora of the studied localities in the late Ottnangian regional stage (upper part of the Burdigalian). Additionally, these age data indicate that deposition of the overlaying Salgotarjan Formation starts much later than originally thought (during Ottnangian-Karpatian boundary).","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-05-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43789100","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 4
Pre-Variscan granitoids with adakitic signature at west Getic basement of the South Carpathians (Romania): constraints on genesis and timing based on whole-rock and zircon geochemistry 南喀尔巴阡山脉(罗马尼亚)西Getic基底具有阿达基期特征的华力西前花岗质岩石:基于全岩和锆石地球化学的成因和时间限制
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-04-14 DOI: 10.1344/GEOLOGICAACTA2021.19.4
A. Dobrescu
Research on two strata-like intrusions from Slatina-Timis (STG) and Buchin (BG) at West Getic Domain of the South Carpathians (Semenic Mountains) identified granitoids with adakitic signature in a continental collision environment. Whole-rock geochemical composition with high Na 2 O, Al 2 O 3 and Sr, depleted Y ( 40), (La/Yb) N (>10) ratios and no Eu anomalies overlaps the High-Silica Adakites (HSA) main characteristics, though there are differences related to lower Mg#, heavy metal contents and slightly increased 87 Sr/ 86 Sr ratios. Comparison with HSA, Tonalite-Trondhjemite-Granodiorite (TTG) rocks and melts from experiments on basaltic sources suggests partial melting at pressures exceeding 1.25GPa and temperatures of 800-900oC (confirmed by calculated Ti-in zircon temperatures) as the main genetic process, leaving residues of garnet amphibolite, garnet granulite or eclogite type. The adakitic signature along with geochemical variations observed in the STG-BG rocks indicate oceanic source melts affected by increasing mantle influence and decreasing crustal input that may restrict the tectonic setting to slab melting during a subduction at low angle conditions. An alternative model relates the STG-BG magma genesis to garnet-amphibolite and eclogite partial melting due to decompression and heating at crustal depth of 60-50km during syn-subduction exhumation of eclogitized slab fragments and mantle cumulates. The granitoids were entrained into a buoyant melange during collision and placed randomly between two continental units. U-Pb zircon ages obtained by LA-ICP-MS and interpreted as Ordovician igneous crystallization time and Variscan recrystallization imprint are confirmed by trace-element characteristics of the dated zircon zones, connecting the STG-BG magmatism to a pre-Variscan subduction-collision event. The rich zircon inheritance reveals Neoproterozoic juvenile source and older crustal components represented by Neoarchean to Paleoproterozoic zircons.
通过对南喀尔巴阡山脉(Semenic Mountains)西域Slatina-Timis (STG)和Buchin (BG)两个类地层侵入岩的研究,发现了大陆碰撞环境下具有埃达质特征的花岗岩类。高Na 2o、Al 2o3和Sr、贫Y(40)、(La/Yb) N (bbb10)比值、无Eu异常的全岩地球化学组成与高硅埃达奇岩(HSA)的主要特征重合,但存在Mg#较低、重金属含量较低、87 Sr/ 86 Sr比值略高的差异。玄武岩源实验表明,与HSA相比,tonalite - trondhjemite - grano闪长岩(TTG)岩石和熔体在超过125 gpa的压力和800-900℃的温度下(经ti -锆石计算温度证实)部分熔融是主要的成因过程,残留石榴石角闪岩、石榴石麻粒岩或榴辉岩类型。在STG-BG岩石中观测到的阿达质特征和地球化学变化表明,洋源熔体受到地幔影响增加和地壳输入减少的影响,这可能将构造背景限制在低角度俯冲条件下的板块熔化。另一种模式认为,STG-BG岩浆的成因与60-50km地壳深度的榴辉岩和石榴石角闪岩的部分熔融有关,这是在同步俯冲发掘榴辉岩化的板块碎片和地幔堆积过程中发生的。花岗岩类在碰撞过程中被卷入浮力混杂岩,并随机放置在两个大陆单元之间。LA-ICP-MS得到的U-Pb锆石年龄被解释为奥陶系火成岩结晶时间和瓦里斯坎再结晶印记,并通过锆石测年带的微量元素特征加以证实,将STG-BG岩浆活动与瓦里斯坎前俯冲碰撞事件联系起来。丰富的锆石继承揭示了新元古代幼锆石和以新太古代至古元古代锆石为代表的较古老的地壳成分。
{"title":"Pre-Variscan granitoids with adakitic signature at west Getic basement of the South Carpathians (Romania): constraints on genesis and timing based on whole-rock and zircon geochemistry","authors":"A. Dobrescu","doi":"10.1344/GEOLOGICAACTA2021.19.4","DOIUrl":"https://doi.org/10.1344/GEOLOGICAACTA2021.19.4","url":null,"abstract":"Research on two strata-like intrusions from Slatina-Timis (STG) and Buchin (BG) at West Getic Domain of the South Carpathians (Semenic Mountains) identified granitoids with adakitic signature in a continental collision environment. Whole-rock geochemical composition with high Na 2 O, Al 2 O 3 and Sr, depleted Y ( 40), (La/Yb) N (>10) ratios and no Eu anomalies overlaps the High-Silica Adakites (HSA) main characteristics, though there are differences related to lower Mg#, heavy metal contents and slightly increased 87 Sr/ 86 Sr ratios. Comparison with HSA, Tonalite-Trondhjemite-Granodiorite (TTG) rocks and melts from experiments on basaltic sources suggests partial melting at pressures exceeding 1.25GPa and temperatures of 800-900oC (confirmed by calculated Ti-in zircon temperatures) as the main genetic process, leaving residues of garnet amphibolite, garnet granulite or eclogite type. The adakitic signature along with geochemical variations observed in the STG-BG rocks indicate oceanic source melts affected by increasing mantle influence and decreasing crustal input that may restrict the tectonic setting to slab melting during a subduction at low angle conditions. An alternative model relates the STG-BG magma genesis to garnet-amphibolite and eclogite partial melting due to decompression and heating at crustal depth of 60-50km during syn-subduction exhumation of eclogitized slab fragments and mantle cumulates. The granitoids were entrained into a buoyant melange during collision and placed randomly between two continental units. U-Pb zircon ages obtained by LA-ICP-MS and interpreted as Ordovician igneous crystallization time and Variscan recrystallization imprint are confirmed by trace-element characteristics of the dated zircon zones, connecting the STG-BG magmatism to a pre-Variscan subduction-collision event. The rich zircon inheritance reveals Neoproterozoic juvenile source and older crustal components represented by Neoarchean to Paleoproterozoic zircons.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-04-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47911599","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia) 俄罗斯北西山-乌拉尔山皮姆瓦肖尔河段切尔内雪夫隆起段Timan-Pechora盆地早-中弗拉斯世(晚泥盆世)碳同位素事件
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-04-09 DOI: 10.1344/GEOLOGICAACTA2021.19.3
I. Kotik, Andrey V. Zhuravlev, T. Maydl, D. Bushnev, I. Smoleva
Details of the Early-Middle Frasnian boundary interval of the Pymvashor River section (Timan-Pechora Basin, Cis-Urals, in the far north of European Russia) are revealed by biostratigraphically constrained carbonate (δ 13 C carb ) and organic carbon (δ 13 C org ) stable data. The studied interval corresponds to the lower part of the Domanik Formation, which consists of interbedded limestone and shale beds. Organic-rich black shale that lacks bioturbation and benthic organisms indicates an oxygen-depleted depositional environment. Detection of isorenieratene derivatives in organic matter indicates that anoxia was present in the photic zone during deposition. The Pymvashor River section contains δ 13 C carb  and δ 13 C org  isotope records related to the Early-Middle Frasnian isotope Event. The similarity between the Cis-Uralian (this study) and the Chinese δ 13 C carb  and δ 13 C org  oscillations, including the twostep pattern of the recorded major positive excursions, suggests a robust correlation of the Late Devonian Early- Middle Frasnian isotope Event and minor intra-event excursions. Magnitude of variations and values of δ 13 C org  and δ 13 C carb  in the punctata Zone in the Pymvashor River section are minor than those observed in the North American, Polish, and Chinese successions. Such difference may reflect specific variation of the local environments.
Pymvashor河段(Timan-Pechora盆地,Cis-Urals,位于俄罗斯欧洲北部)早-中Frasnian边界层段的详细信息通过生物地层学约束的碳酸盐岩(δ13C-carb)和有机碳(δ13C-org)稳定数据揭示。所研究的层段对应于Domanik组的下部,该组由石灰岩和页岩夹层组成。缺乏生物扰动和底栖生物的富含有机物的黑色页岩表明沉积环境缺氧。有机物中异renieratene衍生物的检测表明,在沉积过程中,光区存在缺氧。Pymvashor河段包含与早-中Frasnian同位素事件有关的δ13C碳和δ13C有机同位素记录。Cis Uralian(本研究)与中国δ13C carb和δ13C org振荡之间的相似性,包括记录的主要正偏移的两步模式,表明晚泥盆纪-早-中Frasnian同位素事件与小的事件内偏移之间存在强大的相关性。Pymvashor河段punctata带δ13C org和δ13C carb的变化幅度和值小于北美、波兰和中国序列中观察到的变化幅度。这种差异可能反映了当地环境的具体变化。
{"title":"Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)","authors":"I. Kotik, Andrey V. Zhuravlev, T. Maydl, D. Bushnev, I. Smoleva","doi":"10.1344/GEOLOGICAACTA2021.19.3","DOIUrl":"https://doi.org/10.1344/GEOLOGICAACTA2021.19.3","url":null,"abstract":"Details of the Early-Middle Frasnian boundary interval of the Pymvashor River section (Timan-Pechora Basin, Cis-Urals, in the far north of European Russia) are revealed by biostratigraphically constrained carbonate (δ 13 C carb ) and organic carbon (δ 13 C org ) stable data. The studied interval corresponds to the lower part of the Domanik Formation, which consists of interbedded limestone and shale beds. Organic-rich black shale that lacks bioturbation and benthic organisms indicates an oxygen-depleted depositional environment. Detection of isorenieratene derivatives in organic matter indicates that anoxia was present in the photic zone during deposition. The Pymvashor River section contains δ 13 C carb  and δ 13 C org  isotope records related to the Early-Middle Frasnian isotope Event. The similarity between the Cis-Uralian (this study) and the Chinese δ 13 C carb  and δ 13 C org  oscillations, including the twostep pattern of the recorded major positive excursions, suggests a robust correlation of the Late Devonian Early- Middle Frasnian isotope Event and minor intra-event excursions. Magnitude of variations and values of δ 13 C org  and δ 13 C carb  in the punctata Zone in the Pymvashor River section are minor than those observed in the North American, Polish, and Chinese successions. Such difference may reflect specific variation of the local environments.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-04-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45877715","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 4
Middle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinity Zagorje Mid Transdanubian带(Mt.Kuna Gora;克罗地亚西北部)中三叠纪高钾钙碱性渗出岩和火山碎屑岩:矿物学、岩石学、地球化学和构造岩浆亲和力
IF 1.5 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2021-03-04 DOI: 10.1344/GEOLOGICAACTA2021.19.2
Damir Slovenec, B. Šegvić
This study uses mineralogical, petrological, geochemical, and Sr and Nd isotope data along with K-Ar ages to infer the petrogenesis and geodynamic evolution of Middle Triassic high-K calc-alkaline lavas and their associated pyroclastics of Mt. Kuna Gora in NW Croatia. Their analogue mineralogy and bulk-rock geochemistry testify to the coeval origin of both rock types. Sanidine and plagioclase accompanied by inor augite and Ti-bearing magnetite are the major phases found in a matrix of devitrified volcanic glass and plagioclase microlites. Hydrothermal anddiagenetic processes in the pyroclastics originated the formation of chlorite and white mica, and mixed-layer clay minerals, respectively. Petrography reveals the following crystallization order: spinel→clinopyroxene→plagioclase→alkali-feldspar±Fe-Ti oxides. Geochemical and isotopic data suggests that the studied rocks had a complex origin that included the contamination of subduction-generated magmas by lithospheric mantle melts. This presumes an interplay between fertile arc mantle, subducted continental crust, and depleted or ocean island basalts-like mantle. A low degree of crustal contamination stands as a last step in the formation of such “hybrid” magmas. The subducted Paleotethyan oceanic lithosphere went through processes of partial melting at depths of ~45-49km and pressures of ≤1.6GPa and fractionation that produced melts which gave rise to the studied rocks. In the model we are proposing herein such formed partial melts are related to the demise of the northward subduction of the Paleotethys oceanic lithosphere during the Early to Middle Triassic epoch, which is consistent with an active, ensialic mature volcanic arc developing along Laurussian southern active margins.
本研究使用矿物学、岩石学、地球化学、Sr和Nd同位素数据以及K-Ar年龄来推断克罗地亚西北部库纳戈拉山中三叠纪高钾钙碱性熔岩及其相关火山碎屑的岩石成因和地球动力学演化。它们的相似矿物学和大块岩石地球化学证明了这两种岩石类型的同时代起源。在失透火山玻璃和斜长石微晶的基质中发现的主要相是闪长岩和斜长石,并伴有普通辉石和含钛磁铁矿。火山碎屑岩中的热液和沉积过程分别起源于绿泥石和白云母以及混合层粘土矿物的形成。岩石学揭示了以下结晶顺序:尖晶石→单斜辉石→斜长石→碱性长石±铁钛氧化物。地球化学和同位素数据表明,所研究的岩石起源复杂,包括岩石圈地幔熔体对俯冲产生的岩浆的污染。这假设了肥沃的弧地幔、俯冲的大陆地壳和贫化或类似海岛玄武岩的地幔之间的相互作用。低程度的地壳污染是形成这种“混合”岩浆的最后一步。俯冲的古特提斯洋岩石圈在约45-49km的深度和≤1.6GPa的压力下经历了部分熔融和分馏过程,产生了产生所研究岩石的熔体。在我们提出的模型中,这种形成的部分熔体与早三叠纪至中三叠纪期间古特提斯洋岩石圈向北俯冲的消亡有关,这与沿着Laurussian南部活动边缘发育的活跃的、ensialic成熟的火山弧相一致。
{"title":"Middle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinity","authors":"Damir Slovenec, B. Šegvić","doi":"10.1344/GEOLOGICAACTA2021.19.2","DOIUrl":"https://doi.org/10.1344/GEOLOGICAACTA2021.19.2","url":null,"abstract":"This study uses mineralogical, petrological, geochemical, and Sr and Nd isotope data along with K-Ar ages to infer the petrogenesis and geodynamic evolution of Middle Triassic high-K calc-alkaline lavas and their associated pyroclastics of Mt. Kuna Gora in NW Croatia. Their analogue mineralogy and bulk-rock geochemistry testify to the coeval origin of both rock types. Sanidine and plagioclase accompanied by inor augite and Ti-bearing magnetite are the major phases found in a matrix of devitrified volcanic glass and plagioclase microlites. Hydrothermal anddiagenetic processes in the pyroclastics originated the formation of chlorite and white mica, and mixed-layer clay minerals, respectively. Petrography reveals the following crystallization order: spinel→clinopyroxene→plagioclase→alkali-feldspar±Fe-Ti oxides. Geochemical and isotopic data suggests that the studied rocks had a complex origin that included the contamination of subduction-generated magmas by lithospheric mantle melts. This presumes an interplay between fertile arc mantle, subducted continental crust, and depleted or ocean island basalts-like mantle. A low degree of crustal contamination stands as a last step in the formation of such “hybrid” magmas. The subducted Paleotethyan oceanic lithosphere went through processes of partial melting at depths of ~45-49km and pressures of ≤1.6GPa and fractionation that produced melts which gave rise to the studied rocks. In the model we are proposing herein such formed partial melts are related to the demise of the northward subduction of the Paleotethys oceanic lithosphere during the Early to Middle Triassic epoch, which is consistent with an active, ensialic mature volcanic arc developing along Laurussian southern active margins.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.5,"publicationDate":"2021-03-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47139073","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 6
期刊
Geologica Acta
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1