| 高分辨率层序地层学在陆相地层研究中若干问题的讨论 |
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| 引用本文： | 王嗣敏,刘招君.高分辨率层序地层学在陆相地层研究中若干问题的讨论[J].地层学杂志,2004,28(2):179-184. |
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| 作者姓名： | 王嗣敏 刘招君 |
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| 作者单位： | 石油大学,北京,盆地与油藏研究中心,北京,102200;吉林大学地球科学学院,吉林,长春,130061;吉林大学地球科学学院,吉林,长春,130061 |
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| 基金项目： | 中国石油天然气总公司资助项目 |
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| 摘 要： | 高分辨率层序地层学在实际应用中尚存在若干值得注意的问题。理论上要深刻理解基准面概念的涵义,认识到基准面的相对性属性;注意区分地层记录中存在着自旋回和异旋回两种不同成因机制的沉积旋回。在基准面旋回的划分和识别上,原有的短期、中期和长期旋回三级划分方案在定义上过于含糊,易产生歧义,建议以多数学者比较认同的旋回时限进行五级划分为宜。在应用上,以相组合和相序特征为依据划分基准面旋回,避免以粒序特征为凭识别基准面旋回,结合实践提出陆相沉积环境中从冲积平原→深湖相的五级基准面旋回识别模式和实例。
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| 关 键 词： | 高分辨率层序地层学 陆相 基准面 自旋回 异旋回 旋回分级 地层划分 |
| 文章编号： | 0253-4959(2004)02-0179-06 |
| 修稿时间： | 2003年9月12日 |
DISCUSSION ON SOME PROBLEMS OF HIGH RESOLUTION SEQUENCE STRATIGRAPHY IN THE STUDY OF CONTINENTAL STRATIGRAPHY |
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| WANG Si-min,LIU Zhao-jun Basin & Reservoir Research Center,University of Petroleum,Beijing, College of Earth Sciences,Jilin University,Changchun.DISCUSSION ON SOME PROBLEMS OF HIGH RESOLUTION SEQUENCE STRATIGRAPHY IN THE STUDY OF CONTINENTAL STRATIGRAPHY[J].Journal of Stratigraphy,2004,28(2):179-184. |
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| Authors: | WANG Si-min LIU Zhao-jun Basin & Reservoir Research Center University of Petroleum Beijing College of Earth Sciences Jilin University Changchun |
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| Institution: | WANG Si-min,LIU Zhao-jun Basin & Reservoir Research Center,University of Petroleum,Beijing,102200 College of Earth Sciences,Jilin University,Changchun,130061 |
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| Abstract: | There are still some notable problems left in the application of high resolution sequence stratig-
raphy.Theoretically,we should profoundly understand the implication of the conception of base-level and
have a correct understanding of the base-level’s property of relativity.We should pay close attention to
distinguishing two kinds of sedimentary cycles with different genesis mechanisms of autocyclicity and allo
cyclicity.In the classification of base-level cycles,it seems a little bit vague in the definition of the three
order classification scheme of short,medium and long term cycles.It has been suggested that a five-order
base-level cycle classification scheme based on the cycle duration and accepted by most geologists,should
be adopted.Finally,base-level cycle recognition must be based on the features of facies assemblage and fa
cies order,and avoid to recognizing base-level cycle with graded facies.Combined with practical research
work.the author put forward a recognition model of fifth order base-level cycle in the continental sedimen
tary environment. |
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| Keywords: | high resolution sequence stratigraphy continental facies base-level autocyclicity allocyclicity cycle grading recognition model |
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