中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Transformation of accommodation space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China

文献类型:期刊论文

作者Jiang, ZX; Lu, HB; Yu, WQ; Sun, Y; Guan, DS; Jiang, ZX, China Univ Geosci, Coll Energy, 29 Xueyuan Rd, Beijing 100083, Peoples R China
刊名BASIN RESEARCH
出版日期2005-12-01
卷号17期号:4页码:569-582
ISSN号0950-091X
DOI10.1111/j.1365-2117.2005.00275.x
文献子类Article
英文摘要Analysis of accommodation space variation during deposition of the Cretaceous Qingshankou Formation in the Songliao Basin, NE China, indicates that accommodation space changed both through time and across the basin as a seesaw movement. The mid-upper Qingshankou Formation is divided into three units. In each unit, changes of accommodation space differ in the southern and northern part of the basin. Increasing accommodation in the southern part is accompanied by a decrease in the northern part, and vice versa. Between the northern and southern basin, there was a neutral belt that is like a fulcrum, called the transformation belt here, where the accommodation did not change to any significant degree. We call this response 'accommodation transformation', whose characteristics are defined by tectonic subsidence analysis, palaeontological and sedimentary analyses. The accommodation increasing belt, decreasing belt, transformation belt and accommodation transformation boundary together constitute the accommodation transformation system. The recognition of accommodation transformation in the Songliao Basin provides a new insight into sequence stratigraphy and might be widely applicable.; Analysis of accommodation space variation during deposition of the Cretaceous Qingshankou Formation in the Songliao Basin, NE China, indicates that accommodation space changed both through time and across the basin as a seesaw movement. The mid-upper Qingshankou Formation is divided into three units. In each unit, changes of accommodation space differ in the southern and northern part of the basin. Increasing accommodation in the southern part is accompanied by a decrease in the northern part, and vice versa. Between the northern and southern basin, there was a neutral belt that is like a fulcrum, called the transformation belt here, where the accommodation did not change to any significant degree. We call this response 'accommodation transformation', whose characteristics are defined by tectonic subsidence analysis, palaeontological and sedimentary analyses. The accommodation increasing belt, decreasing belt, transformation belt and accommodation transformation boundary together constitute the accommodation transformation system. The recognition of accommodation transformation in the Songliao Basin provides a new insight into sequence stratigraphy and might be widely applicable.
学科主题Geosciences, Multidisciplinary
URL标识查看原文
语种英语
WOS记录号WOS:000233626800006
公开日期2010-11-18
源URL[http://ir.qdio.ac.cn/handle/337002/1825]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Jiang, ZX, China Univ Geosci, Coll Energy, 29 Xueyuan Rd, Beijing 100083, Peoples R China
作者单位1.China Univ Geosci, Coll Energy, Beijing 100083, Peoples R China
2.Shell Int Explorat & Prod Inc, Bellaire Technol Ctr, Houston, TX USA
3.Chinese Acad Sci, Grad Sch, Beijing, Peoples R China
4.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China
5.China Univ Petr, Coll Earth Resource & Informat, Shandong, Peoples R China
6.PetroChina, Res Inst Petr Explorat & Dev, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Jiang, ZX,Lu, HB,Yu, WQ,et al. Transformation of accommodation space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China[J]. BASIN RESEARCH,2005,17(4):569-582.
APA Jiang, ZX,Lu, HB,Yu, WQ,Sun, Y,Guan, DS,&Jiang, ZX, China Univ Geosci, Coll Energy, 29 Xueyuan Rd, Beijing 100083, Peoples R China.(2005).Transformation of accommodation space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China.BASIN RESEARCH,17(4),569-582.
MLA Jiang, ZX,et al."Transformation of accommodation space of the Cretaceous Qingshankou Formation, the Songliao Basin, NE China".BASIN RESEARCH 17.4(2005):569-582.

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来源:海洋研究所

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