| 摘要: |
| 分析总结了海平面及海平面变化的有关问题,如相关概念及其关系的理解,海平面变化旋回等时性及可对比性,海平面升降曲线的表示方法、内容及绘制技术与原理,其升降幅度的定量化计算和模拟,海平面变化成因的旋回级别、动态分异及成因标识,海平面变化对沉积盆地的影响等等。提出部分建议,包括理清海平面与海平面变化,海平面升降与振荡、波动,全球与相对、高频、复合海平面,T-R旋回与海平面变化等概念;限定其概念的外延、内涵及其之间的关系,以及三、四级海平面变化旋回用于同一大陆或泛大陆的对比性;分清各种表示方法、技术的使用范围,相对水深曲线转换为海平面升降曲线过程中成岩作用、构造沉降、沉积(生产)速率的影响校正及定量模拟;在海平面变化旋回级次格架下结合两种思路进行成因分析;推荐相对海平面升降成因分析按曲线对比法→构造沉降→回剥法思路进行;建议加强海平面升降变化对盆地充填响应的研究;重视对沉积矿床的控制和大陆边缘地壳变形的反弹作用过程及定量模拟。 |
| 关键词: 海平面 海平面变化 概念含义和关系 曲线方法 变化成因 充填响应 |
| DOI： |
| 附件 |
| 投稿时间：1998-11-20修订日期：1999-05-17 |
| 基金项目: |
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| Sequence stratigraphic cycles of the third member of the Denglouku Formation in the Xujiaweizi subsidence, Daqing, northeastern China |
| LI Xiang-hun, ZHAO Guo-lian |
| (Department of Reservoir Geophysics, Geophysical Institute of the Chinese Academy of Sciences, Beijing 100101, China) |
| Abstract: |
| The third member of the Denglouku Formation is a prospect area for the oil and gas resources in the Xujiaweizi subsidence, Daqing, northeastern China. In this paper, the lithology and sedimentary facies are discussed, and sequence stratigraphic cycles and their systems tracts are discriminated on the basis of sedimentary facies, lithology and well logs. Hie classification has been verified by using Fischer's plots, which may be a potential tool for sequence analysis. |
| Key words: Xujiaweizi subsidence in Daqing third member of the Denglouku Fonnation sedimentaiy fecies lithology cycle systems tract Fischer's plot |
