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Magnetic fabric of OPS mélanges: a tool for unravelling protracted histories of oceanic plates from sea-floor spreading to tectonic emplacement into accretionary wedges OPS mélanges的磁结构:揭示海洋板块从海底扩张到构造置入增生楔的漫长历史的工具
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-08 DOI: 10.1144/jgs2023-141
Lucia Pellerey, J. Žák, F. Tomek, Andrea Festa
Multiple magnetic fabrics, referred to as F1–F5, were revealed through the anisotropy of magnetic susceptibility (AMS) in an Ocean Plate Stratigraphy (OPS) mélange of the Neoproterozoic–Cambrian Blovice accretionary complex, Bohemian Massif. The fabrics postdate the mélange formation and rotation of basalt blocks within the matrix and are interpreted in terms of a complex structural history of the mélange. Excluding local fabrics, the F1 fabric formed earlier along the mélange belt, recording shortening of the accretionary wedge front, whereas the higher-grade F4 fabric pervasively overprinted both blocks and matrix in the SW part of the belt, recording shearing and vertical shortening at deeper structural levels closer to a megathrust surface. The preservation of angular relationships between the F1 and F4 fabrics across different parts of mélange suggests that blocks were only strained and not rotated during deformation, exemplifying the notion that the OPS mélanges may be a product of deformation at very shallow levels. Finally, the F1–F5 fabrics may be viewed as snapshots in a protracted evolution of OPS mélanges, where earlier fabrics in basalt blocks may record the travel path of an oceanic plate from mid-ocean ridge towards the trench, before being overprinted in the accretionary wedge. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists Supplementary material: https://doi.org/10.6084/m9.figshare.c.7008173
在波希米亚丘陵地带新新生代-寒武纪布洛维采积复合体的海洋板块地层(OPS)中,通过磁感应强度各向异性(AMS)揭示了多个磁性构造,称为 F1-F5。这些织构出现在混杂岩层形成和基质中玄武岩块旋转之后,可从混杂岩层复杂的构造历史角度进行解释。除去局部构造外,F1构造沿熔岩带形成较早,记录了增生楔前沿的缩短,而较高级的F4构造在熔岩带西南部的岩块和基质上普遍覆盖,记录了更深的构造层的剪切和垂直缩短,更接近大地壳表面。F1和F4织物之间的角度关系在混杂带的不同部分都得到了保留,这表明在变形过程中,岩块只受到拉伸而没有发生旋转,这充分说明了OPS混杂带可能是极浅层变形的产物这一观点。最后,F1-F5构造可被视为大洋板块混合岩漫长演化过程中的一个缩影,玄武岩块中的早期构造可能记录了大洋板块从大洋中脊向海沟移动的路径,然后被覆盖在增生楔中。 专题集:本文是蛇绿岩、熔岩和蓝晶岩论文集的一部分,可在以下网址查阅: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists 补充材料:https://doi.org/10.6084/m9.figshare.c.7008173
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引用次数: 0
Interaction of surface processes and crustal flow in the Eastern Himalayan Syntaxis 喜马拉雅山脉东段地表过程与地壳流动的相互作用
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-08 DOI: 10.1144/jgs2023-041
Guangwei Li, Haibin Yang, M. Sandiford, Barry P. Kohn, Zhiqin Xu, Hanwen Dong, Dongxu Cai
The syntaxes at the eastern and western ends of the Himalaya located at the Tsangpo and Indus gorge regions provide examples of the interplay between tectonics and erosion. A previous borehole study along the Yarlung River in the Eastern Himalayan Syntaxis (EHS) reveals a ∼1 km thick sedimentary wedge upstream of the Tsangpo gorge with a >2.5 Ma depositional age. However, mechanism of formation of this sedimentary wedge remains under debate. Here, we combine low-temperature thermochronology data and thermo-mechanical modelling to discuss how a sedimentary wedge formed at the highly eroded EHS. Our low-temperature thermochronology results show late Miocene fast cooling episodes focused at the Gyaca and Tsangpo gorges, which are interpreted to be related to coeval rifting at the former and rapid erosion and hot-crust upwelling at the latter. Constrained by the geological and geophysical observations, we apply thermo-mechanical models to illustrate the mechanism of formation of the sedimentary wedge and present high relief of the EHS. The numerical geodynamic model shows that localised erosion triggers middle ‘crust extrusion’ and regional topographic adjustment at the EHS. Thematic collection: This article is part of the Mesozoic and Cenozoic tectonics, landscape and climate change collection available at: https://www.lyellcollection.org/topic/collections/mesozoic-and-cenozoic-tectonics-landscape-and-climate-change Supplementary material: https://doi.org/10.6084/m9.figshare.c.7008098
位于喜马拉雅山脉东西两端的藏布峡谷和印度河峡谷地区的综合体是构造与侵蚀相互作用的例证。之前在东喜马拉雅轴(EHS)雅鲁藏布江沿岸进行的钻孔研究显示,在藏布峡谷上游有一个厚达 1 千米的沉积楔,沉积年龄大于 2.5 兆年。然而,该沉积楔的形成机制仍存在争议。在此,我们结合低温热年代学数据和热力学模型,讨论了高度侵蚀的东高峰沉积楔是如何形成的。我们的低温热年代学结果显示,中新世晚期的快速冷却事件主要集中在加查峡谷和藏布峡谷,据解释,这与前者的共生断裂以及后者的快速侵蚀和热壳上涌有关。在地质和地球物理观测的限制下,我们应用热力学模型来说明沉积楔的形成机制,并展示了高海拔地区的地貌。数值地球动力学模型显示,局部侵蚀引发了中层 "地壳挤压 "和 EHS 的区域地形调整。 专题文集:本文是中生代和新生代构造、地貌和气候变化文集的一部分,可在以下网址查阅: https://www.lyellcollection.org/topic/collections/mesozoic-and-cenozoic-tectonics-landscape-and-climate-change 补充材料: https://doi.org/10.6084/m9.figshare.c.7008098
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引用次数: 0
Coherent underplating of HP-LT blueschist packages and basement during Hellenic subduction recorded by zircon U-Pb data, Pelion, Greece 锆石U-Pb数据记录的希腊佩利昂HP-LT蓝晶岩包和基底在希腊俯冲过程中的相干下沉过程
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-08 DOI: 10.1144/jgs2023-147
Emily R. Hinshaw, D. Stockli, Kostantinos Soukis
Studies of high pressure-low temperature (HP-LT) metamorphic complexes are critical for advancing our understanding of subduction processes, such as underplating, metamorphism, and exhumation. Detailed new U-Pb zircon data of blueschist-facies metasedimentary units at Pelion indicate two distinct, stratigraphically upright, and coherent structural slices, with (1) the South Pelion slice consisting of strata with Permian-Late Cretaceous zircon maximum depositional ages (MDAs) and (2) the North Pelion slice comprising strata with Triassic-Late Cretaceous zircon MDAs. Both slices have Late Cretaceous strata at the top of the section with cosmopolitan detrital zircon (DZ) signatures. Ages from zircon U-Pb rim overgrowths correlate with existing constraints from subduction-metamorphism during the Paleocene-Eocene, with a possible second stage recorded during Basal underplating in the Late Eocene-Oligocene. DZ provenance data and multi-dimensional scaling (MDS) comparisons demonstrate a tectono-metamorphic linkage between the Pelion rocks and the Cycladic Blueschist Unit (CBU), and between the southern Pelion Basement and the Cycladic Basement (CB). Protolith deposition for Pelion blueschist-facies rocks occurred during Permo-Carboniferous intra-arc extension and Adria-Pindos rifting. Our results show that the Pelion blueschist-facies rocks, representing lateral equivalents of the CBU, are comprised of two separate, coherent upper-crustal slivers that were underplated and metamorphosed during Hellenic subduction beneath the Pelagonian margin. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists Supplementary material: https://doi.org/10.6084/m9.figshare.c.7008123
对高压-低温(HP-LT)变质复合体的研究对于推动我们了解俯冲过程(如欠增层、变质作用和掘起)至关重要。佩利昂蓝岩成因变质岩单元的详细U-Pb锆石新数据表明,有两个不同的、地层直立的、连贯的构造片,其中(1)南佩利昂片由二叠纪-晚白垩世锆石最大沉积年龄(MDAs)的地层组成;(2)北佩利昂片由三叠纪-晚白垩世锆石最大沉积年龄(MDAs)的地层组成。这两个片断的顶部都是晚白垩世地层,具有世界性的碎屑锆石(DZ)特征。锆石 U-Pb 边缘增生的年龄与古新世-始新世期间俯冲变质作用的现有制约因素相关,在晚始新世-渐新世的基底下沉过程中可能有第二阶段的记录。DZ 出处数据和多维尺度(MDS)比较表明,在佩利翁岩石和基克拉迪蓝晶岩单元(CBU)之间,以及在佩利翁基底南部和基克拉迪基底(CB)之间,存在着构造-变质联系。佩利翁蓝晶岩的原岩沉积发生在二叠纪石炭纪弧内延伸和阿德里亚-平多斯断裂时期。我们的研究结果表明,代表CBU横向等值体的佩利昂蓝基岩是由两块独立、连贯的上地壳薄片组成的,它们在佩利昂边缘下方的希腊俯冲过程中发生了下伏和变质作用。 专题文集:本文是蛇绿岩、熔岩和蓝晶岩文集的一部分,可从以下网址获取: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists 补充材料:https://doi.org/10.6084/m9.figshare.c.7008123
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引用次数: 0
Offscraping and shallow ophiolite accretion in the Ligurian Accretionary Wedge (Tuscan Apennines): role of seafloor structural inheritance 利古里亚沉积楔(托斯卡纳亚平宁山脉)的剥蚀和浅蛇绿岩增生:海底结构继承的作用
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-05 DOI: 10.1144/jgs2023-189
G. Nirta, F. Remitti, Edoardo Barbero, A. Festa
The Morello Tectonic Unit in the Tuscan Apennines (Italy) represents the result of tectono-sedimentary deformation, occurring in the frontal part of the non-metamorphosed Ligurian Accretionary Wedge, which consists of ophiolitic slices imbricated with a sedimentary succession containing ophiolite-bearing sedimentary mélanges. Geological mapping, structural and stratigraphic observations, allow us to document that (i) the ophiolite-bearing sedimentary mélanges formed by gravitational reworking of material sourced from intrabasinal structural highs facing the oceanic basin environment from Jurassic to lower Eocene, before the middle Eocene accretion stage, and (ii) the ophiolitic tectonic slices represent the scraping off at shallow structural levels of part of these crustal oceanic highs sequence. The final internal architecture of the shallow frontal portion of the Ligurian Accretionary Wedge does not differ from those observed in metamorphosed orogenic belts and exhumed accretionary complexes throughout the world (e.g., blueschist and eclogite units of Western Alps). This suggests that to the classical model of subduction and metamorphism followed by accretion and mélange formation (i.e., underplating), a model in which frontal accretion and ophiolite mélange formation at a shallow level are followed by underthrusting and subduction can be added, providing additional constraints to a better reconstruction of orogenic belts and accretionary complexes evolution. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
托斯卡纳亚平宁山脉(意大利)的莫雷洛构造单元是构造沉积变形的结果,发生在未变质的利古里亚沉积楔的正面部分,由蛇绿岩切片与含蛇绿岩沉积泥岩的沉积演替交错组成。通过地质测绘、构造和地层学观察,我们发现:(i) 含蛇绿石的沉积泥岩是在中始新世增生阶段之前,对来自侏罗纪至下始新世大洋盆地环境的海盆内构造高地的物质进行重力再加工而形成的;(ii) 蛇绿岩构造切片代表了这些地壳大洋高地序列的一部分在浅构造层面上被刮除。利古里亚增生楔浅锋面部分的最终内部结构与在全世界变质造山带和出露增生复合体(如西阿尔卑斯山的蓝晶岩和绿帘岩单元)中观察到的结构并无不同。这表明,除了传统的俯冲和变质,然后是增生和叠层形成(即欠增生)的模式之外,还可以增加一种模式,即在浅层的锋面增生和蛇绿岩叠层形成之后是欠推和俯冲,从而为更好地重建造山带和增生复合体的演化提供更多的制约因素。 专题文集:本文是蛇绿岩、熔岩和蓝晶岩文集的一部分,可在以下网址查阅:https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists。
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引用次数: 0
Early Jurassic and Late Cretaceous plagiogranites in Nain-Baft ophiolitic mélange zone in Iran: remnants of rift–drift and SSZ evolution of a Neotethyan seaway 伊朗纳因-巴夫特蛇绿岩混杂带的早侏罗世和晚白垩世长花岗岩:新特提安海道的裂谷-漂移和SSZ演化遗迹
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-05 DOI: 10.1144/jgs2023-181
N. Shirdashtzadeh, Y. Dilek, H. Furnes, E. Dantas
We have investigated the geology, geochemistry, and geochronology of various plagiogranite intrusions that are spatially associated with ophiolitic subunits in a mélange terrain exposed within the Nain–Baft fault zone along the western boundary of the Central–East Iranian Microcontinent (CEIM). One group of plagiogranites is intrusive into foliated amphibolites, whereas the plagiogranites of the other group are intrusive into gabbros, dike swarms, and pillow lavas that are tectonically juxtaposed. U–Pb zircon dating of the first group of plagiogranites has revealed near concordant crystallization ages of 176.94±0.71, 179.84±0.92, and 190.40±2.1 Ma, indicating the early Jurassic timing of their emplacement. U–Pb zircon dating of the second group of plagiogranites has revealed a weighted average age of 92.34±0.38 Ma, indicating that they were emplaced in the early Late Cretaceous. The Early Jurassic plagiogranites are low–K, sub–alkaline rocks with negative Eu anomalies, low Ti and high La and Ce contents. They display elevated LILE/HFSE ratios. They were part of a magmatic system which facilitated the earliest rift–drift stages of a Neotethyan seaway development, and their magmas were produced by fractional crystallization of a mafic melt associated with asthenospheric upwelling beneath a rift system. The Late Cretaceous plagiogranites are low–K, sub–alkaline rocks with negative Eu anomalies, high Y and low Ta contents. They show LREE depletion relative to flat HREE patterns, and high Ba/Th ratios. Magmas of these plagiogranites were the products of partial melting of amphibolites in the subducting oceanic lithosphere in the same Neotethyan seaway. Thus, we posit that plagiogranite rocks in suture zones can be excellent trackers of geochemical, geochronological, and magmatic evolution of various types of oceanic crust through rift–drift, seafloor spreading, and subduction initiation stages within the same ocean basins in the past. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
我们对伊朗中部-东部微大陆(CEIM)西部边界纳因-巴夫特断裂带内出露的在空间上与蛇绿岩亚单位相关的各种长花岗岩侵入体的地质、地球化学和地质年代进行了研究。其中一组斜长花岗岩侵入到叶状闪长岩中,而另一组斜长花岗岩则侵入到构造并列的辉长岩、梭状岩群和枕状熔岩中。第一组斜长花岗岩的铀-铅锆石年代测定显示了近乎一致的结晶年龄,分别为 176.94±0.71、179.84±0.92 和 190.40±2.1Ma,表明它们的成岩时间为侏罗纪早期。第二组长花岗岩的U-Pb锆石年代测定显示其加权平均年龄为(92.34±0.38)Ma,表明其成岩时间为晚白垩世早期。早侏罗世长花岗岩是低 K、亚碱性岩石,具有负 Eu 异常、低 Ti 以及高 La 和 Ce 含量。它们显示出较高的 LILE/HFSE 比率。它们是岩浆系统的一部分,该岩浆系统促进了新近纪海道发展的最早裂谷-漂移阶段,其岩浆是由裂谷系统下与星体层上升流有关的黑云母熔体分块结晶产生的。晚白垩世长花岗岩是低K、亚碱性岩石,具有负Eu异常、高Y和低Ta含量。相对于平坦的 HREE 模式,它们显示出 LREE 贫化以及高 Ba/Th 比率。这些斜长花岗岩的岩浆是同一新特提安海道中俯冲洋岩石圈中的闪长岩部分熔融的产物。因此,我们认为缝合带中的长花岗岩可以很好地追踪过去同一大洋盆地内各类大洋地壳在经历裂谷-漂移、海底扩张和俯冲起始阶段的地球化学、地质年代和岩浆演化过程。 专题集:本文是蛇绿岩、熔岩和蓝晶岩文集的一部分,可在以下网址查阅:https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists。
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引用次数: 0
Mississippian olistostromes of Iberia revisited: Tectonic drivers of synorogenic carbonate platform/reef destruction 重新审视伊比利亚的密西西比岩层:同生碳酸盐平台/礁石破坏的构造驱动因素
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-05 DOI: 10.1144/jgs2023-187
Í. F. Dias da Silva, Manuel Francisco Pereira, E. G. Clavijo, José Brandão Silva
A review of the synorogenic basins formed on the Gondwana side of the Variscan orogen of Iberia is presented, highlighting the widespread ocurrence of calciturbiditic formations and olistostromes containing reef-limestone olistoliths in Iberia's Variscan basins. Using key-examples from the Variscan orogen for comparison (Azrou-Khenifra and Rhenohercynian basins), the significance of these olistostromes and flyschoid deposits is discussed. Our tectonic models of the Variscan belt in Iberia propose possible drivers of synorogenic carbonate platform/reef destruction responsible for the origin of calciturbidites and olistostromes. One model proposes the formation of an orogenic plateau by lateral flow of partially molten orogenic roots in the context of Laurussia-Gondwana convergence, following the destruction of the Rheic Ocean and Gondwana (lower) plate slab retreat. An alternative model invokes subduction of Paleotethys oceanic lithosphere beneath the Gondwana (upper) plate. Both emphasize the Mississippian occurrence of a significant thermal anomaly beneath Gondwana that favored strong lithosphere thinning, creating ideal conditions for synorogenic carbonate platform/reef destruction, and for the formation of calciturbidite deposits and olistostromes in Iberia. Variscan paleotopography would look alike in both situations. Thus, distinguishing these models is not straightforward, with differences in the kinematics of the regional tectonic transport in the superstructure of Mississippian gneiss domes. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
本文回顾了伊比利亚瓦里斯坎造山带冈瓦纳一侧形成的同生盆地,重点介绍了伊比利亚瓦里斯坎盆地中广泛存在的钙质透辉石地层和含有礁灰岩鲕粒的鲕粒岩。利用瓦里斯坎造山作用的主要实例(Azrou-Khenifra 和 Rhenohercynian 盆地)进行比较,讨论了这些鲕粒和蝇状沉积的意义。我们对伊比利亚瓦里斯坎带的构造模型提出了造成钙华岩和鲕粒起源的同生碳酸盐平台/礁破坏的可能驱动因素。一种模型认为,在劳鲁西亚-冈瓦纳汇聚的背景下,部分熔融的造山根系通过横向流动形成了造山高原,之后莱茵洋遭到破坏,冈瓦纳(下)板块板块后退。另一种模型则认为冈瓦纳(上)板块下的古特提斯大洋岩石圈发生了俯冲。这两种模式都强调了密西西比时期冈瓦纳板块下方出现了明显的热异常,这有利于岩石圈的强烈减薄,为同生碳酸盐平台/礁的破坏以及伊比利亚方解石沉积和鲕粒的形成创造了理想的条件。在这两种情况下,变石期古地貌看起来都是一样的。因此,由于密西西比时期片麻岩穹隆上部结构的区域构造运移运动学存在差异,要区分这些模式并非易事。 专题文集:本文是蛇绿岩、熔岩和蓝晶岩文集的一部分,可在以下网址查阅:https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists。
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引用次数: 0
Dolomite formation during penecontemporaneous subaerial diagenesis: Evidence from modern dolomite crusts forming in lagoon Brejo do Espinho, Brazil 白云岩在半同期次生成岩过程中形成:巴西 Brejo do Espinho 泻湖中形成的现代白云岩结壳的证据
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-05 DOI: 10.1144/jgs2023-159
Meng Ning, Yao Wang, Judith A. McKenzie, C. Vasconcelos, Chenqing Li, Anjiang Shen, Feng Liang, Bing Shen
Early lithification of carbonate mud during the subaerial exposure stage, under semiarid conditions, has been proposed to facilitate dolomite formation. However, how the biogeochemical processes during subaerial diagenesis promote dolomite formation remains unclear. Here, we employ a multiproxy approach to investigate the process of dolomite formation by analyzing modern dolomite crusts forming in lagoon Brejo do Espinho (LBE). Petrological analysis reveals that the crusts comprise coexisting high-Mg calcite (HMC) and dolomite. Low Fe and Mn concentrations indicate the formation of dolomite under oxic conditions, while a higher Sr concentration in well-lithified crust suggests primary bacterial-induced dolomite precipitation. The Mg isotopic composition of the crusts exhibits a lighter value compared to that of modern sabkha dolomite, suggesting different dolomitization processes and Mg sources. More negative δ ¹³C values of the crusts than unlithified carbonate mud in LBE, indicating the incorporation of 13 C depleted organic carbon. The biogeochemical processes related to decaying organic matter during subaerial diagenesis generate partially oxidized organic matter that promotes Mg 2+ dehydration and enhances the dissolution of primary HMC, ultimately triggering the transition of HMC to dolomite or/and direct dolomite precipitation. The ancient "dolomite factory" operated through cyclic deposition of carbonate sediments and penecontemporaneous subaerial diagenesis. Thematic collection: This article is part of the Towards unravelling the ‘Dolomite Problem’: new approaches and novel perspectives collection available at: https://www.lyellcollection.org/topic/collections/towards-unravelling-the-dolomite-problem
有人提出,在半干旱条件下,亚生代暴露阶段碳酸盐泥的早期岩化可促进白云岩的形成。然而,亚生成岩过程中的生物地球化学过程如何促进白云岩的形成仍不清楚。在此,我们采用多代理方法,通过分析在环礁湖 Brejo do Espinho(LBE)形成的现代白云石结壳,研究白云石的形成过程。岩石学分析表明,结壳由高镁方解石(HMC)和白云石共存组成。铁和锰的浓度较低,表明白云石是在缺氧条件下形成的,而钙锶浓度较高的结壳则表明是由细菌诱导的原生白云石沉淀。与现代sabkha白云岩相比,结壳的镁同位素组成显示出较轻的值,表明白云岩化过程和镁来源不同。结壳的δ ¹³C 负值比 LBE 中未碎石的碳酸盐泥更大,表明 13 C 贫化有机碳的加入。在次生成岩过程中,与有机质衰变有关的生物地球化学过程会产生部分氧化的有机质,从而促进 Mg 2+ 的脱水,并增强原生 HMC 的溶解,最终引发 HMC 向白云岩的转变或/和白云岩的直接沉淀。古代 "白云石工厂 "通过碳酸盐沉积物的循环沉积和半同期次生成岩作用而运行。 专题文集:本文是 "走向解开'白云石问题':新方法和新视角 "专题集的一部分,可在以下网址查阅:https://www.lyellcollection.org/topic/collections/towards-unravelling-the-dolomite-problem。
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引用次数: 0
Late Paleozoic magmatism and foreland deformation associated with opening and closing of marginal basins in the North Patagonian Andes 与北巴塔哥尼亚安第斯山脉边缘盆地开合有关的晚古生代岩浆活动和前陆变形
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-04 DOI: 10.1144/jgs2023-171
C. Rapela, M. García, F. Hervé, R. Pankhurst, M. Calderon, C. Fanning, S. Verdecchia
Remnants of coeval Devonian oceanic and continental foreland rocks are preserved in the basement of the North Patagonian Andes. Our previous studies of igneous rocks have shown the primitive oceanic and continental igneous rocks are coeval, and belong to a marginal basin that opened and closed over 50 Myr. A structural study and four new U-Pb SHRIMP ages and zircon Hf-O determinations allow identification of three metamorphic episodes, the first one M 1 (D 1 -S 1 ) coeval with Andean type granite intrusion in the foreland (405–380 Ma). This activity was simultaneous with development of an oceanic ridge and a marginal basin, at the outer edge of which a primitive granitic oceanic arc formed (380–385 Ma; zircon δ 18 O 3.6–5.2 δ 18 ‰). Ridge extinction initiated under-thrusting of the oceanic crust below the continent and an important mid-to-high grade metamorphic event M 2 (D 2 -S 2; 375–360 Ma), its peak dated by metamorphic zircon rims in migmatite at 365 ± 3 Ma. Basin closure occurred after intrusion of S-type granites (357 ± 2 Ma; zircon δ 18 O 7.4–10.4‰) in the foreland, and accretion of gabbros, cumulate gabbros and trondhjemites at the proto-Pacific margin. Compression prevailed for 20 Myr in the foreland, causing a mylonitic medium-grade M 3 (D 3 -S 3 ) event. Supplementary material: https://doi.org/10.6084/m9.figshare.c.6989873
北巴塔哥尼亚安第斯山脉的基底中保存着共生泥盆纪大洋岩和大陆前陆岩的遗迹。我们之前对火成岩的研究表明,原始的大洋岩和大陆火成岩是共生的,属于一个边缘盆地,其开合时间超过50万年。通过结构研究和四个新的 U-Pb SHRIMP 年龄以及锆石 Hf-O 测定,我们确定了三个变质期,第一个 M 1(D 1 -S 1)与前陆的安第斯型花岗岩侵入期(405-380Ma)同时期。这一活动与洋脊和边缘盆地的发展同时进行,在洋脊和边缘盆地的外缘形成了原始花岗岩洋弧(380-385 Ma;锆石 δ 18 O 3.6-5.2 δ 18 ‰)。海脊的消亡引发了大陆下方大洋地壳的下推,并引发了重要的中高级变质事件M 2(D 2 -S 2;375-360Ma),其峰值被偏闪长岩中的变质锆石边缘测定为365 ± 3Ma。在前陆侵入S型花岗岩(357 ± 2 Ma;锆石δ 18 O 7.4-10.4‰),并在原太平洋边缘增生辉长岩、累积辉长岩和闪长岩之后,盆地开始封闭。前陆的压缩作用持续了20Myr,造成了麦饭石中级M 3(D 3 -S 3)事件。 补充材料:https://doi.org/10.6084/m9.figshare.c.6989873
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引用次数: 0
The Jurassic ophiolitic mélanges in Serbia - a review and new insights 塞尔维亚侏罗纪蛇绿混杂岩--回顾与新见解
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-03 DOI: 10.1144/jgs2023-165
N. Djerić, H. Gawlick, M. Sudar
In Serbia ophiolitic mélanges occur widespread below ophiolites. These ophiolites are interpreted to derive from different oceanic domains and are therefore attributed to different tectonic units. We revisited all existing data from matrix ages and blocks in the mélanges, studied the relictic sedimentological features and dated new sections and blocks from various ophiolitic mélanges. On base of these results we can distinguish three different ophiolitic mélanges: 1. Intra-oceanic ophiolitic mélanges (OM1); 2. Ophiolitic mélanges formed during ophiolite obduction with continental blocks (OM2), and 3. Ophiolitic mélanges with fluviatile transported sedimentary rocks or tectonically incorporated much younger blocks at the base (OM3). These three types of ophiolitic mélanges resemble the polyphase history of shortening and ophiolite emplacement on the wider Adria plate of Serbia. All ophiolitic mélanges contain the same Triassic component spectrum of oceanic sedimentary cover rocks and have similar matrix ages. It can be concluded that all different ophiolites/ophiolitic mélanges derive from the same Triassic-Jurassic oceanic domain, the Neotethys Ocean which western part obducted during Middle-Late Jurassic times on wider Adria. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
在塞尔维亚,蛇绿混杂岩广泛出现在蛇绿岩之下。这些蛇绿岩被解释为来自不同的海洋区域,因此归属于不同的构造单元。我们重新研究了来自混合岩层基质年龄和岩块的所有现有数据,研究了遗迹沉积特征,并对来自不同蛇绿岩混合岩层的新断面和岩块进行了年代测定。根据这些结果,我们可以区分出三种不同的蛇绿混杂岩:1.大洋内部的蛇绿混杂岩(OM1);2. 蛇绿混杂岩与大陆块体在蛇绿混杂岩俯冲过程中形成的混杂岩(OM2);3.在底部有流体搬运沉积岩或构造结合年轻地块的蛇绿混杂岩(OM3)。这三种类型的蛇绿混杂岩与塞尔维亚阿德里亚大板块的缩短和蛇绿岩成岩的多相历史相似。所有蛇绿混杂岩都含有相同的三叠纪海洋沉积覆盖岩成分谱,基质年龄也相似。由此可以得出结论,所有不同的蛇绿混杂岩/蛇绿混杂岩都来自同一个三叠纪-侏罗纪洋域,即新特提斯洋,该洋的西部在中-晚侏罗纪时期被大阿德里亚板块挤压。 专题集:本文是蛇绿岩、熔岩和蓝晶岩资料集的一部分,可在以下网址查阅:https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists。
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引用次数: 0
A salty snapshot: extreme variations in basal erosion patterns preserved in a submarine channel 咸味快照:海底通道中保存的基底侵蚀模式的极端变化
IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-01-03 DOI: 10.1144/jgs2023-006
J. Casagrande, David M. Hodgson, Jeffrey Peakall
Active submarine channel bases are marked by large erosional features, such as knickpoints and plunge pools. Their presence in ancient channel-fills has rarely been documented, meaning their importance in submarine channel morphodynamics requires investigation. Using seismic reflection data calibrated by wells from a buried submarine channel-fill, we document erosional features 100s m long and 10s m deep, here interpreted as knickpoints and a plunge pool, and provide a mechanistic process for their transfer into the stratigraphic record for the first time. Channel incision patterns are interpreted to record a transient uplift in an otherwise subsiding depocentre. Local structural complexities in the channel slope formed zones of preferential scouring. A switch to a depositional regime preserved the irregular channel base inhibiting their upstream migration and smoothing of the channel base. Their formation and preservation record responses to salt tectonics and provide a unique snapshot of the formative processes of an ancient submarine channel. The presence of these exceptional basal scours indicates that headward erosion processes did not operate rapidly, challenging the paradigm that knickpoint migration controls channel evolution. Our results show that the primary erosion of the main channel surface, and long-term channel evolution, are dominated by far more gradual processes.
活跃的海底河道基底有大型侵蚀地貌,如节理点和跌水潭。它们在古河道填土中的存在很少被记录下来,这意味着需要对它们在海底河道形态动力学中的重要性进行研究。我们利用埋藏在海底河道-填土中的水井校准的地震反射数据,记录了长 100 米、深 10 米的侵蚀地貌(在此解释为节理点和跌水潭),并首次提供了它们转移到地层记录中的机理过程。河道切入模式被解释为记录了原本不断下沉的沉积中心的瞬时抬升。河道斜坡的局部结构复杂,形成了优先冲刷区。转为沉积机制后,不规则的河道基底得以保存,从而抑制了它们向上游迁移,并使河道基底变得平滑。它们的形成和保存记录了盐构造的反应,为古代海底河道的形成过程提供了独特的缩影。这些特殊基底冲刷的存在表明,迎头侵蚀过程并不是快速进行的,这对 "节点迁移控制河道演变 "的范式提出了挑战。我们的研究结果表明,主航道表面的主要侵蚀过程以及航道的长期演变过程都是由更为渐进的过程所主导的。
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引用次数: 0
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Journal of the Geological Society
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