[an error occurred while processing this directive] ������� 2019, 38(1) 204-214 DOI:   10.3969/j.issn.1004-5589.2019.01.019  ISSN: 1004-5589 CN: 22-1111/P

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PubMed
Article by Wang L
Article by Liu Z
Article by Liu D
Article by Wang L
Article by Yue Q
Article by Chi H
Article by Ma X
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1. �й�ʯ�ͼ������﹫˾��������̽�о�Ժ, ���� ��ԭ 138000;
2. ���ִ�ѧ�����ѧѧԺ, ���� 130061;
3. ��������ѧԺ, ���� 130061
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Depiction on volcanic edifice of Yingcheng Formation in Dehui fault depression and its reservoir significance
WANG Li-wu1, LIU Zhi-jun1, LIU Dian-mi1, WANG Li-li1, YUE Qing-you2, CHI Huan-zhao2,3, MA Xiao1
1. Geophysical Exploration Institute, PetroChina Jilin Oilfield Company, Songyuan 138000, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China;
3. Changchun Institute of Technology, Changchun 130061, China
Abstract: Volcanic reservoirs in the Dehui fault depression mainly occurred in volcanic edifice and some in weathering zone. The authors take the inside-type volcanic reservoir as a target and use drilling, logging and seismic data to conduct a detailed description of the internal feature of volcanic edifice, volcanic eruption unit and volcanic facies. Eight volcanic reservoir-types are summarized by observations of cores and thin sections, and the influences of volcanic edifice, eruption unit and facies on volcanic reservoir are analyzed in combination with reservoir physical properties. The results show that the volcanic reservoirs are mainly distributed in the center of volcanic edifice or near crater, the reservoir in the upper part of the eruption unit is better than that in the lower part. Cracks are well developed in the central part of the eruption unit, forming a complete set of pore-crack combination. The favorable volcanic facies for good quality reservoirs are eruptive thermal clastic flow, the upper effusive and the inner invade subfacies.
Keywords: Dehui fault depression   Yingcheng Formation   volcanic edifice   eruption unit   volcanic facies   reservoir  
�ո����� 2018-05-05 �޻����� 2018-12-10 ����淢������  
DOI: 10.3969/j.issn.1004-5589.2019.01.019
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