平衡剖面技术与地震资料解释
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摘要
地质剖面形成至今，一般都经历了数千百万年乃至数亿年的构造形变过程。但其面积（体积）、地层厚度、各标志层的长度在变形前后保持相等，即变形前后的剖面是平衡的。根据这些原则制作的平衡剖面可以作为检验地质构造解释是否正确合理的标准。本文简要介绍了平衡剖面技术及其发展，并论述了平衡剖面技术的正演法和复原法及其在地质解释中的应用。
Generally speaking,geological section has undergone structural deformation for several million years to several hundred million years. But the area, bed thickness and marker bed length remain unchanged ;that is to say,the geological section keeps balanced before and after deformation. The balanced section plotted according to the principle can serve as the standard by which we can verify whether the interpretation of geological structure is reasonable. We sketch out balanced section technique and its development. We also describe the forward and backward methods of balanced section technique,and their applications in geological interpretation.
Generally speaking,geological section has undergone structural deformation for several million years to several hundred million years. But the area, bed thickness and marker bed length remain unchanged ;that is to say,the geological section keeps balanced before and after deformation. The balanced section plotted according to the principle can serve as the standard by which we can verify whether the interpretation of geological structure is reasonable. We sketch out balanced section technique and its development. We also describe the forward and backward methods of balanced section technique,and their applications in geological interpretation.
引文
1陈伟等.平衡剖面计算机模拟及其应用,科学出版社,1993
2 Dahlstrom CDA.Balanced Cross Sections.Canadian Journal of Earth Seience,1969,6:743～757
3 Vans Mount,John Suppe et al.A forward modeling strategy for balancing cross sections.AAPG,1990,74 (5):521～531
4肖安成.平衡剖面的正演模拟方法.江汉石油学院学报,1994,16(1):1～10
5 P B Jones等.利用计算机平衡剖面勘探构造-地层远景带.国外油气勘探,1993,5(4):407～489
6 Rowan M G.有助于张性岩区地震解释的横剖面复原和均衡.国外油气勘探,1990,2(3):17～27
7牟中海.应用地震资料建立压性盆地平衡剖面.石油地球物理勘探,1992,27(4):498～504
8石人骥译.剖面复原和均衡作为地震解释的一种辅助手段.SEG第59届年会论文集,石油工业出版社, 1991:935～936
9 John H Shaw,Stephen C Hooka,John Suppe.Structural trend analysis by axial surface mapping.AAPG, 1994,79(5):700～721
10岳石.国外逆冲构造学的进展概述.国外地质,1991,6:1～3
11严又生译.GEOSEC-提高地震解释的可能性,石油地球物理勘探参考资料,1993,210(9):1～3
12 Mitra S.Fault-propagation folds:geometry,kinematic evolution and hydrocarbon traps.AAPG,1990,74: 921～945
13Bally A W.Seismic expression of Structural styles.AAPG,1984
14 Mitra S.Equal-area balancing.American Journal of Science,1989,289:563～599
15平衡剖面计算机辅助设计软件——LOCACE.石油物深信息(报),1993年11月15日
16平衡剖面技术专题研讨会.石油消息(报),1994年4月16日
17张性盆地构造演化模拟系统(OSESM).石油地震地质,1992,4:封2
2 Dahlstrom CDA.Balanced Cross Sections.Canadian Journal of Earth Seience,1969,6:743～757
3 Vans Mount,John Suppe et al.A forward modeling strategy for balancing cross sections.AAPG,1990,74 (5):521～531
4肖安成.平衡剖面的正演模拟方法.江汉石油学院学报,1994,16(1):1～10
5 P B Jones等.利用计算机平衡剖面勘探构造-地层远景带.国外油气勘探,1993,5(4):407～489
6 Rowan M G.有助于张性岩区地震解释的横剖面复原和均衡.国外油气勘探,1990,2(3):17～27
7牟中海.应用地震资料建立压性盆地平衡剖面.石油地球物理勘探,1992,27(4):498～504
8石人骥译.剖面复原和均衡作为地震解释的一种辅助手段.SEG第59届年会论文集,石油工业出版社, 1991:935～936
9 John H Shaw,Stephen C Hooka,John Suppe.Structural trend analysis by axial surface mapping.AAPG, 1994,79(5):700～721
10岳石.国外逆冲构造学的进展概述.国外地质,1991,6:1～3
11严又生译.GEOSEC-提高地震解释的可能性,石油地球物理勘探参考资料,1993,210(9):1～3
12 Mitra S.Fault-propagation folds:geometry,kinematic evolution and hydrocarbon traps.AAPG,1990,74: 921～945
13Bally A W.Seismic expression of Structural styles.AAPG,1984
14 Mitra S.Equal-area balancing.American Journal of Science,1989,289:563～599
15平衡剖面计算机辅助设计软件——LOCACE.石油物深信息(报),1993年11月15日
16平衡剖面技术专题研讨会.石油消息(报),1994年4月16日
17张性盆地构造演化模拟系统(OSESM).石油地震地质,1992,4:封2
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