塔里木盆地麦盖提斜坡玉北地区奥陶系油气输导体系与成藏期

斯尚华; 陈红汉; 谭先锋; 李纯泉; 吴悠; 李楠

doi:10.3799/dqkx.2013.124

Volume 38 Issue 6

Jun. 2013

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Article Navigation > Earth Science > 2013 > 38(6): 1271-1280

SI Shang-hua, CHEN Hong-han, TAN Xian-feng, LI Chun-quan, WU You, LI Nan, 2013. Hydrocarbon Accumulation Period and Its Carrier Systems in Ordovician Reservoir of Yubei Area, Markit Slope Tarim Basin. Earth Science, 38(6): 1271-1280. doi: 10.3799/dqkx.2013.124

Citation:

SI Shang-hua, CHEN Hong-han, TAN Xian-feng, LI Chun-quan, WU You, LI Nan, 2013. Hydrocarbon Accumulation Period and Its Carrier Systems in Ordovician Reservoir of Yubei Area, Markit Slope Tarim Basin. Earth Science, 38(6): 1271-1280. doi: 10.3799/dqkx.2013.124

Citation:

SI Shang-hua, CHEN Hong-han, TAN Xian-feng, LI Chun-quan, WU You, LI Nan, 2013. Hydrocarbon Accumulation Period and Its Carrier Systems in Ordovician Reservoir of Yubei Area, Markit Slope Tarim Basin. Earth Science, 38(6): 1271-1280. doi: 10.3799/dqkx.2013.124

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Hydrocarbon Accumulation Period and Its Carrier Systems in Ordovician Reservoir of Yubei Area, Markit Slope Tarim Basin

doi: 10.3799/dqkx.2013.124

1.
School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
School of Petroleum Engineering, Chongqing University of Science & Technology, Chongqing 401331, China

Received Date: 2013-01-21
Publish Date: 2013-06-01

Abstract

Abstract

Three types of basic carrier systems are identified for analyzing the hydrocarbon migration and accumulation process of Ordovician reservoir in Yubei area, Southwest Tarim Basin, which are known as fault type, unconformity type and carrier layer type, where the carrier ability is strong in the Middle Part of Yubei area but weak in the Eastern Part. The organic and inorganic fluid inclusion analyses of 25 Ordovician samples from 3 wells in Yubei area indicate that there were two phases of hydrocarbon charging in Ordovician. In the period from 262 Ma to 252 Ma before present (in Late Hercynian), low-mature oil with yellow fluorescence was charged. In the second period from 12.5 Ma to 0 Ma before present (in Late Himalayan), high-maturity oil with blue-white fluorescence was charged. Two groups of hydrocarbon source rocks, namely, the Lower Cambrian source rock and the Upper Cambrian-Lower Ordovician source rock, are developed in Yubei area. The cover is the mudstone and marl of Lower Carboniferous Bachu Formation Strata. The reservoir is the karst weathering of Lower-Middle Ordovician Strata. The cover and reservoir are composed of discontinuous interlayer combinations.
- inclusions,
- hydrocarbon charging events and ages,
- carrier systems,
- Ordovician,
- Yubei area,
- oil bearing formation

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Hydrocarbon Accumulation Period and Its Carrier Systems in Ordovician Reservoir of Yubei Area, Markit Slope Tarim Basin

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