2013, 32(4) 793-799 DOI: ISSN: 1004-5589 CN: 22-1111/P | |||||||||||||||||||||||||||||||||||||||||||||||
Current Issue | Archive | Search [Print] [Close] | |||||||||||||||||||||||||||||||||||||||||||||||
���� |
| ||||||||||||||||||||||||||||||||||||||||||||||
��elationship of Cretaceous volcanic activities and fracture combination in Xujiaweizi fault depression | |||||||||||||||||||||||||||||||||||||||||||||||
YIN Chang-Hai-1, DONG Jing-Hai-2 | |||||||||||||||||||||||||||||||||||||||||||||||
1. Exploration and Development ��esearch Institute of Daqing Oilfield��Daqing 163712��Heilongjiang��China; 2. Exploration Division of Daqing Oilfield��Daqing 163712��Heilongjiang��China | |||||||||||||||||||||||||||||||||||||||||||||||
Abstract��
The authors pointed out that Cretaceous volcanic activities were controlled by the basement faults and secondary faults in Xujiaweizi��and formed three NNW �� trend volcanic rock belts controlled by basement faults��through the study on the relationship among fracture combination��volcanic mechanism and karst channels�� Due to the different characteristics of the basement faults��the volcanic rock belts had three eruption characteristics: center��fracture��and compound in type�� The careful dissection of Xujiaweizi fault depression in Anda area showed that: the NWW �� trend echelon fractures developed in upper basement fractures and communicated the basement faults downward��which were the volcanic magma invasion routes in western area�� These phenomenon reflected the volcanic activity stronger in the west than in the east in the history period��i. e�� the volcanic scale was larger in the west��charactered by burst facies��while showed effusive facies in the east�� The distribution of volcanic rocks were controlled by basement faults and secondary faults��which also played a remolding part to fracture trace�� | |||||||||||||||||||||||||||||||||||||||||||||||
Keywords�� Xujiaweizi fault depression Anda area fracture volcanic (magma) activities volcanic erup- tion mode | |||||||||||||||||||||||||||||||||||||||||||||||
Received Revised Online: | |||||||||||||||||||||||||||||||||||||||||||||||
DOI: | |||||||||||||||||||||||||||||||||||||||||||||||
Fund: | |||||||||||||||||||||||||||||||||||||||||||||||
Corresponding Authors: | |||||||||||||||||||||||||||||||||||||||||||||||
Email: | |||||||||||||||||||||||||||||||||||||||||||||||
About author: | |||||||||||||||||||||||||||||||||||||||||||||||
| |||||||||||||||||||||||||||||||||||||||||||||||
References�� | |||||||||||||||||||||||||||||||||||||||||||||||
Similar articles | |||||||||||||||||||||||||||||||||||||||||||||||
1�� BAI Xue-Feng.Fracture characteristics of volcanic reservoir in Yingcheng Formation , Songliao Basin[J]. , 2009,28(3): 318-325 | |||||||||||||||||||||||||||||||||||||||||||||||
2�� LI Nan, CHENG Lin-Song, LIAN Pei-Qing, CHENG Jia.Cause of hydraulic fractures in carbonate reservoir with abnormal high pressure[J]. , 2011,30(1): 56-59 | |||||||||||||||||||||||||||||||||||||||||||||||
3�� LI Jin-Quan, HAN Li-Guo, LUO Jin-Mei, DANG Dan, QIAO Zhen-Min-.Method of fracture detection based on attenuation coefficient of qp wave and qs wave[J]. , 2011,30(2): 282-288 | |||||||||||||||||||||||||||||||||||||||||||||||
4�� HUANG Wei, WANG Zhi-Guo, DONG Jing-Hai, ZHOU Yue.Application of seismic data for forecasting hydrocarbon source rocks in Shahezi Formation of Xujiaweizi fault depression[J]. , 2013,32(3): 571-578 | |||||||||||||||||||||||||||||||||||||||||||||||
Copyright by |