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We first report discovery of the spinel-garnet-orthopyroxene granulite with pure CO2 fluid inclusions from the Fuyun region of the late Paleozoic Altay orogenic belt in Central Asia, NW China. The rock is characterized by an assemblage of garnet, orthopyroxene, spinel, cordierite, biotite, plagioclase and quartz. Symplectites of orthopyroxene and spinel, and orthopyroxene and cordierite indicate decompression under UHT conditions. Mineral chemistry shows that the or-thopyroxenes have high XMg and A12O3 contents (up to 9.23 wt%). Biotites are enriched in TiO2 and XMg and are stable under granulite facies conditions. The garnet and quartz from the rock carry monophase fluid inclusions which show peak melting temperatures of around -56.7℃, indicating a pure CO2 species being presented during the ultrahigh-T metamorphism in the Altay orogenic belt. The inclusions homogenize into a liquid phase at temperatures around 15.3-23.8℃ translating into CO2 densities of the order of 0.86-0.88 g/cm3. Based on prelim 相似文献
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INTRODUCTION Due to granulites representing products of thedeeper lower crust-upper mantle and having geneticassociation with early crustal evolution and forma-tion of large-scale metallogenic-forming and nonmetallogenic-forming belts, the study of granulitesin the world has resulted in much recent attention(Zhai and Liu, 2001; Liu and Zhou, 1994; Yu et al.,1998; 2003; Li et al., 2000; Zhang et al., 2001; Yuet al., 2002; Bingen and Stein, 2003; Blein et al.,2003; Garcia et al., … 相似文献
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在实验室里,常用加热氯酸钾(用二氧化锰做催化剂)或高锰酸钾的方法来制取氧气。用这种方法制取氧气,操作比较复杂,又不便控制反应,增加了教师课前准备氧气的难度。若改用过氧化氢制取氧气,则操作简便。 相似文献
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We first report discovery of the spinel-garnet-orthopyroxene granulite with pure CO2 fluid inclusions from the Fuyun region of the late Paleozoic Altay orogenic belt in Central Asia, NW China. The rock is characterized by an assemblage of garnet, orthopyroxene, spinel, cordierite, biotite, plagioclase and quartz. Symplectites of orthopyroxene and spinel,and orthopyroxene and cordierite indicate decompression under UHT conditions. Mineral chemistry shows that the orthopyroxenes have high XMg and Al2O3 contents (up to 9.23 wt%). Biotites are enriched in TiO2 and XMg and are stable under granulite facies conditions. The garnet and quartz from the rock carry monophase fluid inclusions which show peak melting temperatures of around -56.7 ℃, indicating a pure CO2 species being presented during the ultrahigh-T metamorphism in the Altay orogenic belt. The inclusions homogenize into a liquid phase at temperatures around 15.3-23.8℃ translating into CO2densities of the order of 0.86-0.88 g/cm3. Based on preliminary mineral paragenesis, reaction textures and petrogenetic grid considerations, we infer that the rock was subjected to UHT conditions. The CO2-rich fluids were trapped during exhumation along a clockwise P-T path following isothermal decompression under UHT conditions. 相似文献
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Hydrocarbon charging histories of the Ordovician reservoir in the Tahe oil field, Tarim Basin, China
INTRODUCTION Researches on hydrocarbon charging historyare essentially important to exploration and de-velopment, especially for the reservoirs subject tomultiple hydrocarbon generations, discharges, mi-grations and accumulations, as was the case of theOrdovician reservoir of the Tahe oil field located atthe southwest slope of the Akekule uplift, TarimBasin, China. Regarding the hydrocarbon charginghistories of the Ordovician reservoir, previousstudies based on burial histories (Y… 相似文献
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本文先简介服务利润链理论,后运用该理论探讨提高我国移动通讯企业获利能力的对策。 相似文献
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文章针对武汉城市圈存在的产业结构层次低、圈内产业结构不均衡、产业同构现象严重等问题,分析了如何从主导产业和产业布局两个方面优化武汉城市圈产业结构。 相似文献
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本文主要针对武汉承接国际制造业转移的劣势，如产业结构不合理、制造业企业竞争力不足、人才流失严重、技术创新能力差、金融服务对制造业支持不够、中介服务体系不完善等进行分析，探讨武汉承接国际制造业转移的制约性，为武汉创造条件承接国际制造业转移，促进产业结构调整，带动地方经济发展提供参考。 相似文献