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| 走滑拉分断块对沉积的控制作用——准噶尔盆地东部侏罗系中下统沉积主控因素新认识 | |
| 引用本文： | 张塞,赵霞飞. 走滑拉分断块对沉积的控制作用——准噶尔盆地东部侏罗系中下统沉积主控因素新认识[J]. 矿物岩石, 1998, 0(Z1) |
| 作者姓名： | 张塞 赵霞飞 |
| 作者单位： | 成都理工学院石油系 |
| 摘 要： | 通过在南缘露头剖面相构型识别，北部地震剖面解释的沉积体侧向迁移特征，建立了走滑拉分构筑的可容空间变化型式。此沉积对构造的响应模式，不仅可以很好的解释拼合砂体的分布，古流向偏转等问题，而且对于预测盆内沉积体走向也是一个很有用的工具。 |
| 关 键 词： | 走滑拉分 可容空间变化 拼合砂体 沉积体走向预测 |
THE REACTION OF SEDIMENTARY CAUSED BY STRIKE SLIP PULL APART FAULT BLOCK:FROM LOWER MIDDLE JURASSAIC THE EAST ZHUNGEER (JUNGGAR) BASIN NORTHWEST CHINA |
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| Zhang Sai Zao Xiafei. THE REACTION OF SEDIMENTARY CAUSED BY STRIKE SLIP PULL APART FAULT BLOCK:FROM LOWER MIDDLE JURASSAIC THE EAST ZHUNGEER (JUNGGAR) BASIN NORTHWEST CHINA[J]. Journal of Mineralogy and Petrology, 1998, 0(Z1) | |
| Authors: | Zhang Sai Zao Xiafei |
| Abstract: | Based on the recognition of facies architecture on the south outcrop and the interpretation of lateral sediments migration on seismic profiles of north slope,the change of sedimentary accumulation formed by strike slip pull apart fault can be estublished . This sedimentary tectonic reaction model gives not only a good explanation for the rotating of Paleocurrent derection but also a usefull tool to predict the derection of sedmentary body in the center of basin. |
| Keywords: | strik slip pull apart the change of sedimentary accumulation amagmated sand body paleocurrents sediments direction |
| 本文献已被 CNKI 等数据库收录！ | |