收稿日期: 1997-12-09
修回日期: 1998-01-09
网络出版日期: 1998-08-01
基金资助
中国有色金属工业总公司矿产地质研究院. 新疆达坂城铜矿找矿远景研究. 1996.
THE DISCOVERY OF LARGE-SCALE INTERLAYER HYDRAULIC FRACTURING SYSTEMS IN BOGEDA RIFT, EASTEN TIAN MOUNTAIN
Received date: 1997-12-09
Revised date: 1998-01-09
Online published: 1998-08-01
汪劲草,王建业,王正云,耿文辉,肖龙 . 东天山博格达裂谷发现大规模层间水力断裂系统[J]. 地球科学进展, 1998 , 13(4) : 403 -406 . DOI: 10.11867/j.issn.1001-8166.1998.04.0403
Interlayer hydraulic fracturing fault, which associated with the fluid activity of wide scope in the depth of sedimentary basins, have been confirmed to develop largely in the Mesozoic and Cenozoic sedimentary basins through the methods of geophysics and drolling sampling. The studies in this paper indicate that large-scale interlayer hydrofracturing clastic rocks, which formed in folded Late Paleozoic rift basin, are the geological trace of fluid face zone and its hydrofracturing in the developing process of sedimentary basins. Author studies its geological feature, forming condition and structure fluid dynamics model, and realizes that the studies above have vital important geological significance in the bed seperation of upper crust, nappe, fluid conductivity, polytype mineralization, oil gas movement, slow earthquake and conventional earthquake, etc.
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