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The Timeline of Two-Stage Accretionary Processes in Eastern Central Asian Orogenic Belt: Insights from Episodic Paleozoic Intrusions in Central Inner Mongolia, North China 中亚东部造山带两期增生时间:内蒙古中部古生代幕式侵入岩的启示
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.3054
Lingling Yuan, Xiaohui Zhang, Zhili Yang
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引用次数: 1
Is it Moving? – The Occurrence and Migration of Gas in Salt Rocks 它在动吗?——盐岩中天然气的赋存与运移
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.2470
B. Strauch, M. Zimmer, A. Zirkler
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引用次数: 0
Thermally Induced Brine Migration in Salt 盐中热致盐水运移
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.518
M. Dangelmayr, H. Boukhalfa, F. Caporuscio, Phillip Stauffer
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引用次数: 0
Molybdenum Isotope Fractionation in Tibet Magmatism 西藏岩浆活动中的钼同位素分馏
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.1549
Yu-Hsuan Liang, Der-Chuen Lee, Sun‐Lin Chung
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引用次数: 0
Lawsonite (Pseudomorph)-Bearing Eclogites from the Kamieniec Metamorphic Belt (Sudetes, SW Poland) 波兰西南部苏台德地区Kamieniec变质带含铁榴辉岩(拟形)
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.1134
S. Ilnicki, J. Szczepański, Xin Zhong
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引用次数: 0
Evolution of Helium Signatures from Kermadec Arc Under Water Volcanoes Kermadec弧水下火山氦特征演化
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.2705
M. Walter, Andreas Türke, C. Mertens, J. Sültenfuss
Method The isotopic signature R = He/He of primordial helium in hydrothermal fluids and plumes is significantly different from the atmospheric ratio (Ra) and can be identified with high precision in fluid/water samples. During the RV Sonne expedition SO253, we sampled noble gas isotopes from four hydrothermal active volcanoes along the Kermadec arc (SW Pacific) with summit depths between 290 to 1200m below the surface. We extend an existing time series of helium isotopes from the 1990s/2000s in this area [1-4] to observe changes in the underlying plumbing of the hydrothermal systems. The samples were analysed in the lab post-cruise using a combined QMS/SMS [5]. Primordial excess He is reported as δHe, the deviation of R from Ra (in %).
方法热液流体和羽流中原始氦的同位素特征R = He/He与大气比值Ra有显著差异,可在流体/水样中进行高精度识别。在SO253年的RV Sonne考察中,我们在Kermadec弧(西南太平洋)的四个热液活火山上采集了稀有气体同位素,这些火山的峰顶深度在地表以下290 ~ 1200m之间。我们扩展了该地区自20世纪90年代至21世纪初的现有氦同位素时间序列[1-4],以观察热液系统下卧管道的变化。样品在巡航后使用QMS/SMS组合在实验室进行分析[5]。原始超额He用δHe表示,即R与Ra的偏差(单位为%)。
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引用次数: 0
Sourcing Metals in Seafloor Hydrothermal Systems: A Research Legacy of Steve Scott 海底热液系统中的金属来源:史蒂夫·斯科特的研究遗产
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.949
M. Hannington
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引用次数: 0
Geochemical Study of Cliff Sediments from the Central Ganga Plain: Implications on Paleoclimate and Depositional History 恒河平原中部悬崖沉积物地球化学研究:古气候和沉积史意义
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.2958
M. Yadav, Anupam Sharma, U. Shukla
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引用次数: 0
Preliminary Geochemical Study of Puyango Deposit, Ecuador, Applying Statistics 厄瓜多尔Puyango矿床地球化学初步研究——应用统计学
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.1717
J. Manrique, J. Ortiz
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引用次数: 0
Assessment of Groundwater Ages Using Radiocarbon and Chlorofluorocarbons in West Hawai'i Aquifer Systems 使用放射性碳和氯氟烃评估西夏威夷含水层系统的地下水年龄
Pub Date : 2020-01-01 DOI: 10.46427/gold2020.1987
B. Okuhata, A. El-Kadi, H. Dulai, Jonghyun Lee, Donald Thomas, B. Popp
1Department of Earth Sciences, University of Hawai‘i at Mānoa, Honolulu, HI 96822, USA (*correspondence: bokuhata@hawaii.edu) 2 Water Resources Research Center, University of Hawai‘i at Mānoa, Honolulu, HI 96822, USA 3 Department of Civil and Environmental Engineering, University of Hawai‘i at Mānoa, Honolulu, HI 96822, USA 4 Hawai‘i Institute of Geophysics and Planetology, University of Hawai‘i at Mānoa, Honolulu, HI 96822, USA
1夏威夷大学地球科学系Mānoa,美国檀香山HI 96822(*通信:bokuhata@hawaii.edu) 2夏威夷大学水资源研究中心Mānoa,美国檀香山HI 96822 3夏威夷大学土木与环境工程系Mānoa,美国檀香山HI 96822 4夏威夷大学地球物理与行星研究所Mānoa,美国檀香山HI 96822
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引用次数: 0
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Goldschmidt Abstracts
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