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Paleoseismology of the Ganos segment; the western extend of the North Anatolian Fault (Turkey) 加诺斯段古地震学;北安纳托利亚断层(土耳其)的西延
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1850
M. Aksoy, M. Meghraoui, M. Ferry, Z. Çakır, G. Uçarkuş, T. Sançar, M. Altın
Recommended Citation AKSOY, MURAT ERSEN; MEGHRAOUI, MUSTAPHA; FERRY, MATTHIEU; ÇAKIR, ZİYADİN; UÇARKUŞ, GÜLSEN; SANÇAR, TAYLAN; and ALTIN, MEHMET UĞUR (2023) "Paleoseismology of the Ganos segment; the western extend of the North Anatolian Fault (Turkey)," Turkish Journal of Earth Sciences: Vol. 32: No. 3, Article 10. https://doi.org/10.55730/1300-0985.1850 Available at: https://journals.tubitak.gov.tr/earth/vol32/iss3/10
AKSOY, MURAT ERSEN;MEGHRAOUI,穆斯塔法;渡轮,马修;CAKIR Zİ雅İN;UCARKUŞGULSEN;SANCAR TAYLAN;和ALTIN, MEHMET UĞUR (2023)加诺斯段古地震学;北安纳托利亚断层(土耳其)的西延伸,《土耳其地球科学杂志》,第32卷,第3期,第10条。https://doi.org/10.55730/1300-0985.1850可在https://journals.tubitak.gov.tr/earth/vol32/iss3/10找到
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引用次数: 0
Internal deformation of continental blocks within converging plates: insights from the Ovacık Fault (Anatolia, Türkiye) 收敛板块内大陆块体的内部变形:来自Ovacık断层(安纳托利亚,土耳其)的启示
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1849
Cengiz Zabcı, T. Sançar, D. Tikhomirov, S. Ivy‐Ochs, C. Vockenhuber, A. Friedrich, Müge Yazıcı, N. Akçar
: The active tectonics of Anatolia is mostly characterized by its westward motion with respect to Eurasia between the Hellenic subduction in the west and Arabia-Eurasia continental collision in the east. Although most of the deformation is suggested to be confined along Anatolia’s boundary elements, viz. the North and East Anatolian shear zones, recent studies indicate a higher magnitude of internal strain accumulation, especially along the parallel/subparallel strike-slip faults of its central province. We present the first morphochronology-based slip rate estimate for one of these strike-slip structures, the Ovacık Fault, by using cosmogenic 36 Cl dating of offset fluvial deposits. At the Köseler Site (39.3643°N, 39.1688°E), two faulted risers, bounding the alluvial fan with its subplanar surface (NF1/NF1’) and the inset terrace tread (NF1/T2), are offset 19–24 and 15–22 m, respectively. The scattered surface ages and variability of 36 Cl concentrations in depth profiles suggest strong evidence for inheritance in alluvial fan and terrace deposits; thus, we used modelled depth-profile ages for both surfaces. The modelled ages 8–10 ka for NF1 and 6–8 ka for T2 yield slip-rate estimates 2.4 +0.5/–0.4 mm/a and 2.8 +0.7/–0.7 mm/a, respectively, for the upper-tread reconstruction of the NF1/NF1’and the lower-tread reconstruction of the NF1/T2. Our results together with previous slip-rate estimates for other structures show a significant internal deformation for Anatolia, especially along its subparallel strike-slip faults. These secondary faults slice Anatolia into several pieces giving rise to the formation of the Malatya-Erzincan, Cappadocian, and Central Anatolian slices, where the geometry is strongly controlled by the distribution of the Tethyan accretionary complexes.
安纳托利亚活动构造的主要特征是相对于欧亚大陆向西运动,在西部的希腊俯冲和东部的阿拉伯-欧亚大陆碰撞之间。虽然大部分变形被认为局限于安纳托利亚的边界元素,即北安纳托利亚剪切带和东安纳托利亚剪切带,但最近的研究表明,内部应变积累的程度更高,特别是沿其中部省份的平行/次平行走滑断层。我们提出了第一个基于形态年代学的滑移率估计,其中一个走滑构造,Ovacık断层,利用宇宙成因36 Cl定年的冲积河流矿床。在Köseler站点(39.3643°N, 39.1688°E),两条断裂的立沟将冲积扇及其亚平面(NF1/NF1′)与插入的阶地踏面(NF1/T2)相结合,分别偏移19 ~ 24 m和15 ~ 22 m。36 Cl浓度在深度剖面上的分散地表年龄和变异性为冲积扇和阶地沉积的遗传提供了强有力的证据;因此,我们对两个表面都使用了模拟深度剖面年龄。在NF1/NF1的上踏面重建和NF1/T2的下踏面重建中,NF1/NF1和T2的屈服滑移率分别为2.4 +0.5/ -0.4 mm/a和2.8 +0.7/ -0.7 mm/a,模型年龄分别为8-10 ka和6-8 ka。我们的结果与先前对其他构造的滑动率估计一起显示了安纳托利亚的显著内部变形,特别是沿着其次平行走滑断层。这些次级断层将安纳托利亚切割成几块,形成了马拉提亚-埃尔津坎、卡帕多西亚和安纳托利亚中部的断层,这些断层的几何形状受到特提斯增生复合体分布的强烈控制。
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引用次数: 0
Relationship of petrographic and mineralogical characteristics with mechanical strength properties of granitic rocks: a case study from the Biga Peninsula, NW Turkey 花岗岩岩相矿物学特征与岩石力学强度的关系——以土耳其西北部比加半岛为例
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1831
Güven Eroğlu, Ayten Çalık
: This study was carried out on granitic rocks from the Biga Peninsula in order to investigate petrographic, and mineralogical properties in comparison with mechanical strength properties. This study was conducted in four different locations where granitic rocks outcrop from north to south in the Biga Peninsula: Lapseki (Şevketiye granite), Ezine (Kestanbol granite), Bayramiç (Yassıbağ granite), and Edremit (Eybek granite). Field observations and detailed petrographic studies of representative samples indicate that they are quartz monzodiorite (Şevketiye and Yassıbağ), quartz monzonite (Kestanbol), and granodiorite (Eybek) in composition. All the rocks have similar mineral composition, comprising mainly feldspar (plagioclase–alkali feldspar), quartz, mafic minerals (biotite and amphibole), accessory minerals (sphene, zircon, opaque minerals), and secondary minerals (sericite, epidote, chlorite) with differences in the percentage of modal mineralogy, textural details, and weathering. Physical and mechanical properties were also defined in this study, these include water absorption, porosity, uniaxial compressive strength (UCS), tensile strength (TS), Schmidt hardness tests (SHT), Los Angeles test (LA), and frost resistance test (FRT) with sodium sulfate (Na 2 SO 4 ). The results of strength tests show that the Şevketiye granite had the lowest strength values with the highest values for Los Angeles abrasion, frost resistance, water absorption, and porosity. The Eybek granite exhibited the highest value for strength, with the lowest values for Los Angeles abrasion, frost resistance, water absorption, and porosity. A comparison of the petrographic properties of all studied rocks with their respective strengths show that modal mineralogy, degree of alteration, and texture influence the strength of the rocks. Additionally, an increasing propensity for UCS and TS values was found with increasing SHT values. The LA abrasion values and the FRT values were found to increase with decreasing Schmidt hardness test values for the tested samples. The found results of this study could help in the application of these rocks as row material.
:这项研究是在比加半岛的花岗岩上进行的,目的是研究岩相和矿物学特性与机械强度特性的比较。这项研究在比加半岛从北到南的四个不同位置进行:Lapseki(Şevketiye花岗岩)、Ezine(Kestanbol花岗岩)、Bayramiç(Yassıbağ花岗岩)和Edremi(Eybek花岗岩)。现场观察和对代表性样品的详细岩相研究表明,它们的成分为石英二长闪长岩(Şevketiye和Yassıbağ)、石英二长岩(Kestanbol)和花岗闪长岩。所有岩石的矿物成分相似,主要包括长石(斜长石-碱性长石)、石英、镁铁质矿物(黑云母和角闪石)、副矿物(sphene、锆石、不透明矿物)和次生矿物(绢云母、绿帘石、绿泥石),但模式矿物学、结构细节和风化作用的百分比不同。本研究还定义了物理和机械性能,包括吸水性、孔隙率、单轴抗压强度(UCS)、拉伸强度(TS)、施密特硬度试验(SHT)、洛杉矶试验(LA)和硫酸钠(Na2SO4)的抗冻性试验(FRT)。强度测试结果表明,Şevketiye花岗岩的强度值最低,洛杉矶耐磨性、抗冻性、吸水性和孔隙率最高。Eybek花岗岩的强度值最高,洛杉矶耐磨性、抗冻性、吸水性和孔隙率值最低。所有研究岩石的岩相特性与其各自强度的比较表明,模式矿物学、蚀变程度和纹理会影响岩石的强度。此外,随着SHT值的增加,UCS和TS值有增加的趋势。发现测试样品的LA磨损值和FRT值随着施密特硬度测试值的降低而增加。这项研究的发现可能有助于将这些岩石用作排料。
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引用次数: 3
Paleoseismology of the Sürgü and Çardak faults - splays of the Eastern Anatolian Fault Zone, Türkiye 东安纳托利亚断裂带Sürgü和Çardak断裂带的古地震学,[j]
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1851
Musa Balkaya, H. Akyüz, Süha Özden
: The sinistral East Anatolian Fault Zone (EAFZ) and the dextral North Anatolian Fault Zone (NAFZ) are two important strike-slip faults that delimit the boundaries of the Anatolian plate. The north-south directed compressional forces in eastern Türkiye trigger the westward escape of the Anatolian plate along these prominent structures. This study aims to reveal the earthquake history of the Sürgü and Çardak faults, which are important fault segments that splay from the EAFZ. In this context, overall, four paleoseismologic trenches were dug, two trenches on the Sürgü Fault and two trenches on the Çardak Fault. Along the Sürgü Fault, at least two paleoearthquake events have been determined on the trench walls, one event occurred around 3400 BCE and the second event happened between 2085 ± 65 BCE and 790 ± 20 BCE. Moreover, trenching results from the Çardak Fault indicate two surface rupturing paleoearthquakes between 10520 ± 95 BCE and 5780 ± 65 BCE, and between 3215 ± 125 BCE and 825 ± 55 CE, respectively. The focal mechanisms of important instrumental earthquakes around the Sürgü and Çardak faults on the EAFZ show that NNE-SSW trending compressional forces are actively dominating the tectonic setting of the region in the contemporary era. Paleoseismological investigations suggested that the Sürgü and Çardak faults have the potential to produce surface-rupturing earthquakes with an estimated magnitude of 7 or larger.
:左旋东安纳托利亚断层带(EAFZ)和右旋北安纳托利亚断裂带(NAFZ)是界定安纳托利亚板块边界的两条重要走滑断层。土耳其东部南北方向的挤压力触发了安纳托利亚板块沿着这些突出结构向西逃离。本研究旨在揭示Sürgü和Çardak断层的地震历史,这两条断层是从EAFZ开始张开的重要断层段。在这种情况下,总共挖掘了四条古地震学海沟,其中两条在Sürgü断层上,两条在Çardak断层上。沿着Sürgü断层,在海沟壁上至少确定了两次古地震事件,一次发生在公元前3400年左右,第二次发生在2085±65至790±20年之间。此外,恰尔达克断层的挖沟结果表明,两次地表破裂古地震分别发生在公元前10520±95和5780±65之间,以及3215±125和825±55之间。EAFZ上Sürgü和Çardak断层周围重要仪器地震的震源机制表明,NNE-SW向挤压力在当代积极主导着该地区的构造环境。古地震学调查表明,Sürgü和Çardak断层有可能产生估计震级为7级或更大的地表破裂地震。
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引用次数: 3
Magnetotelluric investigations over geothermal provinces of India: an overview 印度地热省份大地电磁调查综述
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1835
Prabhala Bhakhara Venkata Subbarao, Pachigolla Venkata Vijaya Kumar, D. Chandrasekharam, Vasu Deshmukh, Ashutosh Kumar Singh
: Magnetotelluric (MT) and audio-magnetotelluric (AMT) studies are sensitive to the geothermal fluids filling the faults and/ or fracture zones of the geothermal system. In India, MT/AMT studies have been carried out in NW Himalayas, central, eastern, and western India. In other areas, detailed MT/AMT studies need to be expedited. This review paper presents the art of geothermal exploration in India by using MT/AMT techniques and identifies potential zones that can be exploited for power generation and direct application. Reservoir characteristics, carbon emissions reduction methods, and levelised cost factor are also discussed.
:大地电磁(MT)和音频大地电磁(AMT)研究对填充地热系统断层和/或断裂带的地热流体很敏感。在印度,在喜马拉雅山脉西北部、印度中部、东部和西部进行了MT/AMT研究。在其他领域,需要加快详细的MT/AMT研究。本文介绍了印度利用MT/AMT技术进行地热勘探的艺术,并确定了可用于发电和直接应用的潜在区域。还讨论了水库特性、碳减排方法和平准成本因素。
{"title":"Magnetotelluric investigations over geothermal provinces of India: an overview","authors":"Prabhala Bhakhara Venkata Subbarao, Pachigolla Venkata Vijaya Kumar, D. Chandrasekharam, Vasu Deshmukh, Ashutosh Kumar Singh","doi":"10.55730/1300-0985.1835","DOIUrl":"https://doi.org/10.55730/1300-0985.1835","url":null,"abstract":": Magnetotelluric (MT) and audio-magnetotelluric (AMT) studies are sensitive to the geothermal fluids filling the faults and/ or fracture zones of the geothermal system. In India, MT/AMT studies have been carried out in NW Himalayas, central, eastern, and western India. In other areas, detailed MT/AMT studies need to be expedited. This review paper presents the art of geothermal exploration in India by using MT/AMT techniques and identifies potential zones that can be exploited for power generation and direct application. Reservoir characteristics, carbon emissions reduction methods, and levelised cost factor are also discussed.","PeriodicalId":49411,"journal":{"name":"Turkish Journal of Earth Sciences","volume":null,"pages":null},"PeriodicalIF":1.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46764389","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
New Triassic finding in Andız Peninsula (İzmir, Western Turkey) and comparison of pre-Neogene sequences of Andız and Karaburun Peninsulas: Stratigraphic and tectonic implications Andız半岛(土耳其西部伊兹密尔)的三叠纪新发现以及Andı
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1858
I. Işintek
Abstrac t: This study aims to review the geology of the Andız Peninsula and compare the pre-Neogene Andız succession with the middle part of the Karaburun Peninsula to discuss the nature of the Paleozoic-Mesozoic boundary in the Karaburun Peninsula. The pre-Neogene units of the Andız Peninsula are represented by the Paleozoic Dikendağı, Triassic Güvercinlik, and Jurassic Nohutalan Formations. In this study, the Triassic carbonate rocks in the Andız Peninsula are paleontologically defined for the first time. The Megalodont-bearing Güvercinlik Formation contains a late Norian-Rhaetian characteristic foraminiferal assemblage consisting of Aulotortus gr. sinuosus , A. tenuis , A. friedli , A. impressus , and Triasina hantkeni . The Thaumatoporella- bearing Nohutalan Formation conformably overlies the Güvercinlik Formation and yields a typical Liassic fossil assemblage of Orbitopsella praecursor, Siphovalvulina gibralterensis, S. colomi, Meandrovoluta asiagoensis , and Palaeodasycladus mediterraneus . In the Andız Peninsula, the Mesozoic Güvercinlik and Nohutalan Formations tectonically overlie the Paleozoic Dikendağı Formation along a displacement contact . In the middle Karaburun Peninsula, the Triassic Gerence Formation lies directly on the Dikendağı Formation along a displacement contact. Lateral continuation of this displacement contact is discovered between the Triassic Gerence and Camiboğazı Formations at the top and Paleozoic Dikendağı Formation at the bottom. Further north, the same displacement contact extends into the Paleozoic sequence where the Carboniferous Alandere Formation tectonically overlies the Dikendağı Formation. These observations suggest that the succession in the Karaburun Peninsula ranging from Bashkirian to Cretaceous, is a tectonic slice or a package of slices over the Dikendağı Formation
摘要本文通过对Andız半岛地质的回顾,并将其前新近系Andız序列与卡拉布润半岛中部进行对比,探讨卡拉布润半岛古生代-中生代界线的性质。Andız半岛前新近系以古生代Dikendağı组、三叠纪gvercinlik组和侏罗系Nohutalan组为代表。本文首次对Andız半岛的三叠系碳酸盐岩进行了古生物鉴定。含巨齿兽的g vercinlik组具有挪威-雷蒂亚晚期特征的有孔虫组合,包括Aulotortus ger . sinusus、a . tenuis、a . friedli、a . impressus和Triasina hantkeni。含thaumatoporela的Nohutalan组整合覆盖在g vercinlik组上,形成了典型的Liassic化石组合,包括Orbitopsella的前身、Siphovalvulina gibralterensis、S. colomi、Meandrovoluta asiagoensis和paleodasycladus mediterraneus。在Andız半岛,中生代 vercinlik组和Nohutalan组沿位移接触构造上覆于古生代Dikendağı组之上。在卡拉布润半岛中部,三叠系成烃组沿置换接触直接位于Dikendağı组之上。在顶部的三叠系和Camiboğazı组与底部的古生代Dikendağı组之间发现了这种位移接触的横向延续。再往北,同样的位移接触延伸到古生代层序,石炭系Alandere组在构造上覆盖Dikendağı组。这些观察结果表明,卡拉布伦半岛从巴什基良到白垩纪的演替是Dikendağı组上的一个构造切片或一系列切片
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引用次数: 0
A local earthquake tomography on the EAF shows dipping fault structure EAF的局部地震层析成像显示出倾斜断层结构
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1845
S. E. Güvercin
: The East Anatolian Fault Zone (EAFZ) is a left-lateral transform fault zone located between the Anatolian and Arabian plates. In this study, in order to image the upper crustal structure beneath the eastern segments of EAFZ, 3D seismic velocity variations are computed using local earthquake tomography. The initial catalog for the tomography process consists of 2200 well-located earthquakes recorded at 49 seismic stations around the study region between 2007 and 2020. 1D initial velocity model is constructed based on previous studies in the region. The maximum number of iterations and the velocity perturbations which sustain the linearity of the inversion are determined based on the detailed tests. Reliable zones of the final model are decided based on the Derivative Weighted Sum and Hit Count distribution. The resulting velocity model displays a clear velocity contrast across the surface trace of the EAFZ down to a depth of 12 km. While the Anatolian side of the fault displays higher velocities associated with the ophiolitic units in the region, the south of the fault zone is represented by lower velocities due to sedimentary deposits. The vertical cross-sections of tomographic models show a north dipping fault between Palu and Çelikhan. The complete earthquake catalog is relocated using the 3D velocity model. Together with the obtained velocity model, the relocated hypocenters indicate that the dip of the EAFZ is not uniform, the Palu segment dips to the north with an angle of ~80°, while the Pütürge and Erkenek segments dip to the north with a lower angle of ~60–70°.
:东安纳托利亚断层带(EAFZ)是一个位于安纳托利亚板块和阿拉伯板块之间的左旋转换断层带。在本研究中,为了对EAFZ东段下方的上部地壳结构进行成像,使用局部地震层析成像计算了三维地震速度变化。层析成像过程的初始目录包括2007年至2020年间在研究区域周围的49个地震站记录的2200次位置良好的地震。在前人研究的基础上,建立了一维初速度模型。基于详细的测试来确定维持反演线性的最大迭代次数和速度扰动。最终模型的可靠区域是基于导数加权和和命中计数分布来确定的。由此产生的速度模型在EAFZ的表面轨迹上显示出明显的速度对比,深度为12 km。虽然断层的安纳托利亚一侧显示出与该地区蛇绿质单元相关的较高速度,但断层带南部由于沉积矿床而表现出较低的速度。断层模型的垂直截面显示了巴鲁和切利汗之间的向北倾斜断层。使用三维速度模型重新定位完整的地震目录。与获得的速度模型一起,重新定位的震源表明EAFZ的倾角不均匀,Palu段向北倾斜约80°,而Pütürge和Erkenek段向北倾斜较低的角度约60–70°。
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引用次数: 0
Petrological characteristics of gabbroic intrusions in southeastern Urmia-Dokhtar magmatic belt, Kerman province, Iran: Evidence for post-Eocene mafic magmatism 伊朗克尔曼省Urmia-Dokhtar岩浆带东南部辉长岩侵入体的岩石学特征:后始新世镁铁质岩浆作用的证据
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1856
Zahra Najafi, H. Ahmadipour, A. Moradian, F. Sarjoughian, K. Nakashima
: At the south of the Bardsir, Kerman province, Iran, the southeastern part of the Urmia-Dokhtar magmatic arc (UDMA), a large number of gabbroic intrusions are intruded into the Eocene lava flows and pyroclastic rocks with the form of small stocks and dykes. In this paper, geochemical variations, magmatic evolutions, and the origin of these intrusions are investigated. The studied intrusions are characterized by fine-grained margins resulting from rapid cooling and flow differentiation. They display porphyritic texture and include coarse-grained clinopyroxene with diopside compositions (Wo = 46.89, En = 40.78, Fs = 12.32), plagioclase with labradorite composition (An = 54.14), and olivine in an intergranular crystalline groundmass. Their whole-rock chemistry proves that the rocks belong to the calc-alkaline series. The abundances of trace elements and REE, depletion of Nb, Ta, Zr, Ti, and Hf, and enrichment of LILE relative to HFSE indicate that these rocks belong to a subduction zone setting. Geochemical characteristics (Sm/Yb and La/Sm ratios) show that the source rock of these intrusions was the lithospheric mantle with spinel lherzolite composition, which initially underwent partial melting (10% to 20%) events and then was metasomatized by fluids derived from the subducting Neo-Tethys lithosphere.
:在伊朗克尔曼省Bardsir的南部,Urmia-Dokhtar岩浆弧(UDMA)的东南部,大量辉长岩侵入体以小型岩堆和岩脉的形式侵入始新世熔岩流和火山碎屑岩中。本文对这些侵入体的地球化学变化、岩浆演化和成因进行了研究。所研究的侵入体的特征是快速冷却和流动分化产生的细粒边缘。它们显示出斑状结构,包括透辉石成分的粗粒斜辉石(Wo=46.89,En=40.78,Fs=12.32)、拉布拉多岩成分的斜长石(An=54.14)和粒间结晶基质中的橄榄石。他们的全岩化学证明这些岩石属于钙碱性系列。微量元素和REE的丰度、Nb、Ta、Zr、Ti和Hf的贫化以及LILE相对于HFSE的富集表明这些岩石属于俯冲带环境。地球化学特征(Sm/Yb和La/Sm比值)表明,这些侵入体的源岩是由尖晶石二辉橄榄岩组成的岩石圈地幔,最初经历了部分熔融(10%至20%)事件,然后被俯冲新特提斯岩石圈的流体交代。
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引用次数: 1
New geodetic constraints on the role of faults and blocks vs. distribute strain in the Nubia-Arabia-Eurasia zone of active plate interactions 努比亚-阿拉伯-欧亚板块活动相互作用带断层和块体作用的新大地测量约束与分布应变
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1842
S. Ergintav, M. Floyd, D. Paradissis, H. Karabulut, P. Vernant, F. Masson, I. Georgiev, A. Konca, U. Doğan, Robert W. King, R. Reilinger
: We present a broad view of present-day motions and deformations derived from uniform processing of GNSS observations within the Nubia-Arabia-Eurasia zone of plate interaction. The new observations we present provide a ~29% increase in the number of velocity determinations, a reduction in average station spacing from ~76 km to ~39 km, and an improvement in velocity uncertainties (for <1 mm/year), from 180 to 578 sites compared to our prior published solution (Reilinger et al., 2006). We use these new constraints to better evaluate the role of faults and blocks in controlling the character of continental deformation within the zone of plate interactions. Simple elastic block models show that internal deformation of the region occurs in large part on mapped, seismically active fault systems, indicating elastic behavior of the seismogenic crust (above ~15 km). For example, eastern central Anatolia, an area of > ~126,000 km 2 , bounded by the North and East Anatolian Faults exhibits internal velocity differences of <0.5 mm/year, indicating strain rates of < ~1.5 nanostrain/year. Geodetically constrained fault slip rates obtained from this simplified approach are comparable to geologic rates, indicating that major faults have controlled the recent geologic evolution of the region (i.e. 5–10 Myr). The pattern of present-day deformation, including increasingly fast motions towards the Hellenic trench, and the roughly simultaneous opening of all the major Mediterranean basins in the early Miocene with the slowing of the Nubia-Eurasia convergence, support conceptual models that foundering and rollback of the subducted Nubian slab beneath the Aegean is the primary mechanism responsible for present-day motion and internal deformation of the Anatolian-Aegean region.
我们对努比亚-阿拉伯-欧亚板块相互作用区域内GNSS观测数据的统一处理得出的现今运动和变形进行了广泛的观察。我们提出的新观测提供了~29%的速度测定数量增加,平均站间距从~76 km减少到~39 km,并且速度不确定性有所改善(在~126,000 km 2中,以北安纳托利亚断层和东安纳托利亚断层为边界,内部速度差<0.5 mm/年,表明应变率< ~1.5纳米应变/年)。这种简化方法得到的受大地测量约束的断层滑动速率与地质速率相当,表明主要断层控制了该地区最近的地质演化(即5-10迈拉)。现今的变形模式,包括越来越快的向希腊海沟移动,以及中新世早期所有主要地中海盆地几乎同时开放,努比亚-欧亚大陆辐合速度减慢,支持了爱琴海下俯冲的努比亚板块的沉没和回滚是造成安纳托利亚-爱琴海地区现今运动和内部变形的主要机制的概念模型。
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引用次数: 1
Variations in Coupling and Deformation Along the Hellenic Subduction Zone 沿希腊俯冲带耦合与变形的变化
IF 1 4区 地球科学 Q2 Earth and Planetary Sciences Pub Date : 2023-01-01 DOI: 10.55730/1300-0985.1843
M. Floyd, R. King, D. Paradissis, H. Karabulut, S. Ergintav, Kostas Raptakis, R. Reilinger
: GNSS observations in and around the Aegean Sea, Peloponnese
:全球导航卫星系统在爱琴海及其周围的观测,伯罗奔尼撒
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引用次数: 1
期刊
Turkish Journal of Earth Sciences
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