Genetic features of oil source rocks in the tertiary lacustrine evaporites in the Western Qaidam Basin

Qiang Jin

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Genetic features of oil source rocks in the tertiary lacustrine evaporites in the Western Qaidam Basin

机译：柴达木盆地西部湖相蒸发岩油源岩的成因特征。

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来源
《AAPG Bulletin》 |2000年第9期|共1页
作者
Qiang Jin;
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正文语种 eng
中图分类石油、天然气地质与勘探;矿床学;
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1. Genetic features of oil source rocks in the tertiary lacustrine evaporites in the Western Qaidam Basin [J] . Qiang Jin AAPG Bulletin . 2000,第9期

机译：柴达木盆地西部湖相蒸发岩油源岩的成因特征。
2. Biomarker characteristics of hydrocarbon source rocks in saline lacustrine basin: a case study of Paleogene-Neogene strata in the Western Qaidam Basin, western China [J] . Guo Zeqing, Liu Weihong, Liu Chenglin, Carbonates And Evaporites . 2019,第3期

机译：盐水曲线盆地烃源岩的生物标志特征 - 以西部玉马盆地古雄 - 新生地层为例
3. Geochemical Characteristics of the Paleogene and Neogene Saline Lacustrine Source Rocks in the Western Qaidam Basin, Northwestern China [J] . Liu Chenglin, Li Haohan, Zhang Xu, Energy & fuels . 2016,第6期

机译：柴达木盆地西部西部古近系和新近系盐湖相烃源岩的地球化学特征
4. Comparison of hydrocarbon generation simulation of source rocks in close and open system: A case of oil shale from Lower Jurassic in Qaidam Basin, China [C] . Jianzhong Qin, Zhiming Li, Baoquan Liu AAAPG International Conference . 2008

机译：近距开放系统烃源岩烃型仿真的比较：中国柴达木盆地下侏罗素的油页岩案例
5. Temporal and spatial source rock variations and the consequence on crude oil composition in the Tertiary petroleum system of the Uinta Basin, Utah, United States of America. [D] . Mueller, Eric. 1998

机译：美国犹他州Uinta盆地第三纪石油系统中时空烃源岩变化及其对原油成分的影响。
6. Geochemical Signatures and Controlling Factors ofRearranged Hopanes in Source Rocks and Oils from Representative Basinsof China [O] . Yao-Ping Wang, *, Xin Zhan, 2020

机译：地球化学签名与控制因素从代表性盆地重新排列在源岩和油中的荷花中国的
7. Stable carbon isotope compositions of isoprenoid chromans in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin, NW China: Source implications [O] . Zhang, YongDong, Jiang, AiZhu, Sun, YongGe, 2012

机译：西北柴达木盆地新生代盐湖相烃源岩中类异戊二烯色氨酸的稳定碳同位素组成：来源意义

Genetic features of oil source rocks in the tertiary lacustrine evaporites in the Western Qaidam Basin

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