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Correction to: Paleoenvironmental changes across the Paleocene–Eocene boundary in West Central Sinai, Egypt: geochemical proxies 埃及西奈中部古新世-始新世边界的古环境变化:地球化学指标
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-04-09 DOI: 10.1186/s00015-020-00358-2
I. Ghandour
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引用次数: 0
The relation between peak metamorphic temperatures and subsequent cooling during continent–continent collision (western Central Alps, Switzerland) 大陆-大陆碰撞期间最高变质温度与随后冷却之间的关系(瑞士阿尔卑斯山脉中西部)
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-04-06 DOI: 10.1186/s00015-020-00356-4
A. Berger, M. Engi, Silja Erne-Schmid, C. Glotzbach, C. Spiegel, Rick de Goede, M. Herwegh
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引用次数: 10
Paleoenvironmental changes across the Paleocene–Eocene boundary in West Central Sinai, Egypt: geochemical proxies 埃及西奈中部古新世-始新世边界古环境变化:地球化学指标
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-03-20 DOI: 10.1186/s00015-020-00357-3
I. Ghandour
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引用次数: 4
Re-description of the sauropod dinosaur Amanzia (“Ornithopsis/Cetiosauriscus”) greppini n. gen. and other vertebrate remains from the Kimmeridgian (Late Jurassic) Reuchenette Formation of Moutier, Switzerland 瑞士Moutier kimmeridian(晚侏罗世)Reuchenette组蜥脚类恐龙Amanzia(“Ornithopsis/Cetiosauriscus”)greppini n. gen.和其他脊椎动物残骸的重新描述
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-02-24 DOI: 10.1186/s00015-020-00355-5
D. Schwarz, P. Mannion, O. Wings, C. Meyer
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引用次数: 2
The Theodul Glacier Unit, a slab of pre-Alpine rocks in the Alpine meta-ophiolite of Zermatt-Saas, Western Alps Theodul冰川单元,位于西阿尔卑斯泽马特-萨斯阿尔卑斯变质蛇绿岩中的前阿尔卑斯岩石板块
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-02-17 DOI: 10.1186/s00015-020-00354-6
K. Bucher, T. Weisenberger, Sebastian Weber, O. Klemm, F. Corfu
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引用次数: 5
The evolution of the Sesia Zone (Western Alps) from Carboniferous to Cretaceous: insights from zircon and allanite geochronology. 石炭纪至白垩纪塞西亚带(西阿尔卑斯山)的演化:来自锆石和allanite年代学的启示。
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-01-01 Epub Date: 2020-12-07 DOI: 10.1186/s00015-020-00372-4
Alice Vho, Daniela Rubatto, Pierre Lanari, Daniele Regis

Microscale dating of distinct domains in minerals that contain relics of multiple metamorphic events is a key tool to characterize the polyphase evolution of complex metamorphic terranes. Zircon and allanite from five metasediments and five metaintrusive high-pressure (HP) rocks from the Eclogite Micaschist Complex of the Sesia Zone were dated by SIMS and LA-ICP-MS. In the metasediments, zircon systematically preserves detrital cores and one or two metamorphic overgrowths. An early Permian age is obtained for the first zircon rim in metasediments from the localities of Malone Valley, Chiusella Valley and Monte Mucrone (292 ± 11, 278.8 ± 3.6 and 285.9 ± 2.9 Ma, respectively). In the Malone Valley and Monte Mucrone samples, the early Permian ages are attributed to high-temperature metamorphism and coincide with the crystallization ages of associated mafic and felsic intrusions. This implies that magmatism and metamorphism were coeval and associated to the same tectono-metamorphic extensional event. In the Malone Valley, allanite from a metasediment is dated at 241.1 ± 6.1 Ma and this age is tentatively attributed to a metasomatic/metamorphic event during Permo-Triassic extension. Outer zircon rims with a late Cretaceous age (67.4 ± 1.9 Ma) are found only in the micaschist from Monte Mucrone. In metagabbro of the Ivozio Complex, zircon cores yield an intrusive age for the protolith of 340.7 ± 6.8 Ma, whereas Alpine allanite are dated at 62.9 ± 4.2 and 55.3 ± 7.3 Ma. The Cretaceous ages constrain the timing of the HP metamorphic stage. The presence of zircon overgrowth only in the central area of the Eclogite Micaschist Complex is attributed to local factors such as (1) multiple fluid pulses at HP that locally enhanced zircon dissolution and recrystallization, and (2) slightly higher temperatures reached in this area during HP metamorphism.

对含有多变质事件遗迹的矿物中不同区域的微尺度定年是表征复杂变质地体多阶段演化的关键工具。采用SIMS和LA-ICP-MS对塞西亚地区榴辉云母岩杂岩中5种变质沉积岩和5种变质高压岩中的锆石和allanite进行了年代测定。在变质沉积层中,锆石系统地保存了碎屑岩心和一到两个变质生长体。在Malone Valley、Chiusella Valley和Monte Mucrone等地的变质沉积物中,第一个锆石边缘的年龄为早二叠世(分别为292±11、278.8±3.6和285.9±2.9 Ma)。Malone Valley和Monte Mucrone样品的早二叠世年龄归因于高温变质作用,与相关的镁质和长英质侵入体的结晶年龄一致。这表明岩浆活动和变质作用是同时发生的,并与同一构造变质伸展活动有关。在马龙谷中发现的一沉积褐褐岩年龄为241.1±6.1 Ma,初步认为这是二叠纪-三叠纪伸展期的一次交代/变质事件。外锆石边缘的年龄为晚白垩世(67.4±1.9 Ma),仅在Monte Mucrone的云母岩中发现。在Ivozio杂岩的变质长岩中,锆石岩心的侵入年龄为340.7±6.8 Ma,而高寒allanite的侵入年龄为62.9±4.2和55.3±7.3 Ma。白垩纪时代限制了HP变质期的时间。锆石过度生长仅发生在榴辉云母杂岩的中心区域,这主要是由于(1)高压多流体脉冲局部增强了锆石的溶蚀和再结晶作用;(2)高压变质过程中该区域温度略高所致。
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引用次数: 12
The role of the antigorite + brucite to olivine reaction in subducted serpentinites (Zermatt, Switzerland). 俯冲蛇纹岩中辉长岩+水辉石对橄榄石反应的作用(Zermatt,瑞士)。
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2020-01-01 Epub Date: 2020-10-26 DOI: 10.1186/s00015-020-00368-0
Elias D Kempf, Jörg Hermann, Eric Reusser, Lukas P Baumgartner, Pierre Lanari

Metamorphic olivine formed by the reaction of antigorite + brucite is widespread in serpentinites that crop out in glacier-polished outcrops at the Unterer Theodulglacier, Zermatt. Olivine overgrows a relic magnetite mesh texture formed during ocean floor serpentinization. Serpentinization is associated with rodingitisation of mafic dykes. Metamorphic olivine coexists with magnetite, shows high Mg# of 94-97 and low trace element contents. A notable exception is 4 µg/g Boron (> 10 times primitive mantle), introduced during seafloor alteration and retained in metamorphic olivine. Olivine incorporated 100-140 µg/g H2O in Si-vacancies, providing evidence for low SiO2-activity imposed by brucite during olivine growth. No signs for hydrogen loss or major and minor element diffusional equilibration are observed. The occurrence of olivine in patches within the serpentinite mimics the former heterogeneous distribution of brucite, whereas the network of olivine-bearing veins and shear zones document the pathways of the escaping fluid produced by the olivine forming reaction. Relic Cr-spinels have a high Cr# of 0.5 and the serpentinites display little or no clinopyroxene, indicating that they derive from hydrated harzburgitic mantle that underwent significant melt depletion. The enrichment of Mg and depletion of Si results in the formation of brucite during seafloor alteration, a pre-requisite for later subduction-related olivine formation and fluid liberation. The comparison of calculated bulk rock brucite contents in the Zermatt-Saas with average IODP serpentinites suggests a large variation in fluid release during olivine formation. Between 3.4 and 7.2 wt% H2O is released depending on the magnetite content in fully serpentinized harzburgites (average oceanic serpentinites). Thermodynamic modelling indicates that the fluid release in Zermatt occurred between 480 °C and 550 °C at 2-2.5 GPa with the Mg# of olivine varying from 68 to 95. However, the majority of the fluid released from this reaction was produced within a narrow temperature field of < 30 °C, at higher pressures 2.5 GPa and temperatures 550-600 °C than commonly thought. Fluids derived from the antigorite + brucite reaction might thus trigger eclogite facies equilibration in associated metabasalts, meta-gabbros, meta-rodingites and meta-sediments in the area. This focused fluid release has the potential to trigger intermediate depths earthquakes at 60-80 km in subducted oceanic lithosphere.

采尔马特Unterer theodululglacier冰川抛光露头中的蛇纹岩中广泛存在由反长花岗岩+水辉石反应形成的变质橄榄石。橄榄石上生长着海底蛇纹石化过程中形成的遗迹磁铁矿网状结构。蛇纹石化与基性岩脉的岩化有关。变质橄榄石与磁铁矿共生,94 ~ 97 Mg#高,微量元素含量低。一个明显的例外是4µg/g硼(> 10倍于原始地幔),在海底蚀变过程中引入,并保留在变质橄榄石中。橄榄石在si空位中加入了100-140µg/g H2O,这为橄榄石生长过程中水镁石施加的低sio2活性提供了证据。没有观察到氢损失或主要和次要元素扩散平衡的迹象。橄榄石在蛇纹岩中呈斑块状分布,模拟了以前水镁石的非均质分布,而含橄榄石脉网和剪切带则记录了橄榄石形成反应产生的逸出流体的路径。残余Cr尖晶石的Cr值高达0.5,蛇纹岩中几乎没有斜辉石,表明其形成于经历了明显的熔融耗损的水合锆石地幔。镁的富集和硅的亏缺导致了海底蚀变过程中水镁石的形成,这是后期俯冲相关橄榄石形成和流体释放的先决条件。Zermatt-Saas中计算的大块岩石水镁石含量与平均碘含量的蛇纹岩的比较表明,橄榄石形成过程中的流体释放变化很大。根据完全蛇纹石化的哈尔茨布尔岩(平均海洋蛇纹石)中磁铁矿的含量,H2O的释放量在3.4 - 7.2 wt%之间。热力学模型表明,采尔马特的流体释放发生在480°C ~ 550°C之间,温度为2 ~ 2.5 GPa,橄榄石的mg#在68 ~ 95之间变化。然而,从该反应中释放的大部分流体是在狭窄的温度场内产生的
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引用次数: 23
Geochemical constrains on dolomitization pathways of the Upper Jurassic carbonate rocks in the Geneva Basin (Switzerland and France) 日内瓦盆地(瑞士和法国)上侏罗纪碳酸盐岩白云石化途径的地球化学约束
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2019-12-01 DOI: 10.1007/s00015-019-00350-5
Y. Makhloufi, E. Samankassou
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引用次数: 5
Tectonics of the Neuchâtel Jura Mountains: insights from mapping and forward modelling neuch<s:1>特尔侏罗山脉的构造:制图和正演模拟的见解
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2019-12-01 DOI: 10.1007/s00015-019-00349-y
V. Rime, Anna Sommaruga, M. Schori, J. Mosar
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引用次数: 12
Johannes Hämmerli and Nicolas Greber receive the 2018 Paul Niggli Medal Johannes Hämmerli和Nicolas Greber获得2018年Paul Niggli奖章
IF 3.1 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2019-12-01 DOI: 10.1007/s00015-019-00338-1
M. Schönbächler, J. Hermann, J. Hammerli, T. Nägler, N. Greber
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引用次数: 0
期刊
Swiss Journal of Geosciences
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