陕甘宁盆地鄂托克前旗地区奥陶系风化壳的地震正演模型
- 1. 北京石油勘探开发科学研究院,北京 100083;
- 2. 中国科学院兰州地质研究所,兰州 730000
作者简介:
卫延召,男,1969年出生,博士,天然气地质。
- 收稿日期:
1999-06-07
- 刊出日期:
1999-12-10
摘要: 针对鄂托克前旗地区下古生界奥陶系风化壳形态,以二维地震资料为主,辅之以钻井及测井资料,利用概念性地震模型正演法,通过地质模型一模拟响应一实际地震剖面三者的对比分析,初步建立起研究区不同古地貌单元同实际地震测线特征之间的对应关系,并藉此识别掌握了研究区奥陶系古风化壳的单测线特征,对在地震测线上风化壳标志层的标定及奥陶系风化古地貌的恢复都有具有重要意义。
The Study of Morphology of Ordovician Weathered Crust with Conceptual Seismic Model rn Ertuokeqianqi,Ordos Basin
- 1. Research Institute of Petroleum Exploration and Development, Beijing 100083;
- 2. Lanzhou Institute of Geology,chinese Academy of Sciemces, Lanzhou 730000
- Received Date:
1999-06-07
- Publish Date:
1999-12-10
Abstract: The discovery and study of Changqing Gas Field in Ordos Basin has shown the gas exploration prospect of Paleozoic,especially the weathered crust gas reservoir of Ordovician System. Ertuokeqianqi is one of the most favorable regions for gas exploration,and it has been paid much attentions for many years. Mainly based on 2-D seismic data and coupled with drilling and well logging data,we studied and described the seismic characteristics of the morphology of the weathered crust of Ordovician,Ertuokeqanqi,Ordos Basin through geological and seismic models. Firstly,through the study of drills,well logs and :sonic synthetic seismograms,we mastered the characteristic essentials of objective formations-the different conic velocity between upper Paleozoic and lower Paleozoic and the two coal formations and their seismic cha-acteristic .At the same time,we also understood the relations of Lithology and Logging parameters, which lays a foundation for developing seismic models. Furthermore,we divided the shapes of the Ordovician weathered crust into four conceptual models,namely, paleotableland,paleopit, paleovalley and paleoslope. Using these models,we elementarily established the corresponding relations between paleogeomorphology and seismic characteristic with the analysis and comparison of geological models,seismic reflection and practical reflection. We have found that the dis- tance between the lower coal formation and Ordovician weathered crust had important relations with the seismic characteristics. Finally,this research is very valuable to interpret and calibrate the weathered crust of Ordovician system on seismic log and to draw the horizontal maps of the relic Ordovician formation over the M55. The maps might reflect the morphology of the weathered crust,and which is helpful to find Ordovician weathered crust gas reservoir and direct the gas exploration in Ertuokepianqi, Ordos Basin.
卫延召, 冯江, 宋海明, 王多云. 陕甘宁盆地鄂托克前旗地区奥陶系风化壳的地震正演模型[J]. 沉积学报, 1999, 17(S1): 734-741.
引用本文: |
卫延召, 冯江, 宋海明, 王多云. 陕甘宁盆地鄂托克前旗地区奥陶系风化壳的地震正演模型[J]. 沉积学报, 1999, 17(S1): 734-741.
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WEI Yan-zhao, FENG Jiang, SONG Hai-ming, WANG Duo-yun. The Study of Morphology of Ordovician Weathered Crust with Conceptual Seismic Model rn Ertuokeqianqi,Ordos Basin[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 734-741.
Citation: |
WEI Yan-zhao, FENG Jiang, SONG Hai-ming, WANG Duo-yun. The Study of Morphology of Ordovician Weathered Crust with Conceptual Seismic Model rn Ertuokeqianqi,Ordos Basin[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 734-741.
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