摘要
合兴场位于川西坳陷中段,龙泉山逆冲推覆带的北部倾伏端。利用三维可视化技术对合兴场地区的断裂构造进行了解释,从地震层位标定、地层追踪、构造解释、相干体断层解释等方面介绍了三维可视化技术在合兴场地区的应用。
Hexingchang is located in the middle of the west depression of Sichuan,the northern pitching side of Longquan Mountain thrust belt.This paper given an interpretation used three-dimensional visualization technology of the faults in Hexingchang region,And given an introduction of the three-dimensional visualization technology application in Hexingchang region,from seimic calibration,horizon track,structural interpretation and fault intepretion with coherence cube and so on.
引文
[1]叶泰然.川西坳陷合兴场-罗江地区上三叠统须家河组二段致密裂缝性砂岩储层预测.成都理工大学硕士论文,2003.
[2]王振升,丁一萍,王照华,等.利用三维可视化技术解释复杂断裂构造[J].天然气地球科学,2008,19(6).
[3]吴永平,王超.三维相干体技术在三维精细构造解释中的应用[J].断块油气田,2008,15(2).
[4]张军华,王月英,赵勇.C3相干体在断层和裂缝识别中的应用利用[J].地震学报,2004,26(5).
[5]陈国俊,堵素君,陈永昌,等.地震相干体技术及其在构造解释中的应用[J].内蒙古石油化工,2003,2(29).
[6]付雷,田晓冬,闫庆学,等.相干体技术在三维地震资料中的应用[J].世界地质,2000,19(3).
[7]Mike Bahorich,Steve Farmer.3-D seismicdiscontinuity for faults and stratigraphic fes-tures[J].The Leading Edge,1995,10.
[8]John Suppe.Geometry and kinematics offault-bend folding.American Journal ofScience,1983.
[9]Peter B.Jones.Triangle zone geometry,ter-minology and kinematics.Bulletin of Canadi-an petroleum geology,1996,44(2).