Micro fractures and pores in lacustrine shales of the Upper Triassic Yanchang Chang7 Member, Ordos Basin, China
Micro fractures and pores in lacustrine shales of the Upper Triassic Yanchang Chang7 Member, Ordos Basin, China
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鄂尔多斯盆地上三叠统延长长7段湖相页岩微裂缝与孔隙
DOI:
10.1016/j.petrol.2017.03.044
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发表时间:
2017-07
影响因子:
--
通讯作者:
Ping’an Peng
中科院分区:
文献类型:
--
作者:
Wenzheng Zhang;Liqin Xie;Weiwei Yang;Yan Qin;Ping’an Peng
Following the successful exploration of shale oil in North America, China recently started to explore.unconventional oil resources. Industrial shale oil flows were obtained from some strata in lacustrine basins,.especially in the Chang7 Member of the Ordos Basin that may reach 150 barrels a day (e.g., in well Geng 295,.2655 m). So one of the most significant questions now being asked focuses on the shale oil storage within the.reservoir interval. In the present study, five organic rich shale samples were collected from the Chang 7 Member.of the Yanchang Formation in the Ordos Basin and were analyzed by field emission scanning electron.microscopy to characterize pores and fractures in the shales. The results show that microfractures are.predominant storage space for shale oil produced from the Chang 7 Member. Three types of fractures and pores.were recognized, including (i) fractures and pores associated with interstitial organic matter and organic lamina,.(ii) fractures and pores occurring in minerals such as pyrite framboid, mica, and feldspar, and (iii) fractures and.pores that are present along the contact interface of organic matter and minerals. These fractures and pores.were mainly formed by oil generation, tectonic stress, or dissolution. The total organic carbon and brittle.minerals are main factors controlling the abundance of pores and fractures. High total organic carbon and.brittle minerals are favorable for the formation and preservation of pores and fractures in shale. These results.may provide an insight that helps to locate sweet spots for shale oil exploration in Ordos Basin and affect oil.exploration in shales in other lacustrine basins of China.
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DOI:
10.2118/138446-ms
发表时间:
2010
期刊:
--
影响因子:
--
作者:
J. Mullen;J. C. Lowry;K. C. Nwabuoku
通讯作者:
J. Mullen;J. C. Lowry;K. C. Nwabuoku
DOI:
--
发表时间:
2005
期刊:
--
影响因子:
--
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通讯作者:
Zhang Wenzheng
影响因子:
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通讯作者:
P. Wróbel;Sławomir Bała;M. Czyzycki;Magdalena Golasik;T. Librowski;B. Ostachowicz;W. Piekoszewski;A. Surowka;M. Lankosz
影响因子:
3.5
作者:
Ø. Marcussen;B. Thyberg;C. Peltonen;J. Jahren;K. Bjørlykke;J. Faleide
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Ø. Marcussen;B. Thyberg;C. Peltonen;J. Jahren;K. Bjørlykke;J. Faleide
影响因子:
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作者:
Ma Jun
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