File Download
  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Balanced geological section for extensional tectonic basin and its implication: An example from southern Songliao Basin

TitleBalanced geological section for extensional tectonic basin and its implication: An example from southern Songliao Basin
伸展构造盆地的平衡剖面及其构造意义: 以松辽盆地南部为例
Authors
Yan, DPTian, CLMeng, LBZhang, JZZhou, MF
Keywords平衡地质剖面 (Balanced geological section)
伸展盆地 (Extensional basin)
构造变形史 (Deformational history)
两井油田 (Liangjing oilfield)
松辽盆地 (Songliao basin)
Issue Date2003
Citation
Earth Science - Journal Of China University Of Geosciences, 2003, v. 28 n. 3, p. 275-280 How to Cite?
地球科学 - 中国地质大学学报, 2003, 第28卷 第3期, pp. 275-280 How to Cite?
AbstractThe balanced geological sect ion has been widely used for the analysis of orogenic belt, but it is infrequent for ex tensional basins. In this paper, 4 extensional balanced geological sect ion analysis were practiced in Fuyu oil layer of Liangjing , Jilin oilfield, southern Songliao basin with the technology and method, including deformation history restoration, decompaction and erosion restoration. The structure of different ages and the continuous sedimentary sections have been restored. T he result s show that the structural styles possess the characteristics of negative flower structure in the shallow level and ex tensional detachment in deep level. The parameters, including fault growth index, the basin ex tensional history and fault detachment depth, indicate that Late Cretaceous is an important stage for the structure transferring mainly with a strike-slip style before this time and an ex tensional structure and detachment after this time. Therefore, a basin model with twin dynamic property and back-arc characters is proposed.
挤压构造的平衡地质剖面分析已经广泛应用于造山带构造分析, 但伸展构造区的平衡地质剖面分析实例仍然很少. 运用盆地分析的技术与方法, 分层序或阶段将地质构造依次恢复、地层逐层回剥, 并通过在松辽盆地南部吉林两井油田扶余油层4 条剖面的实践, 复原出不同时代盆地构造与地层发育的连续剖面, 揭示出松辽盆地南部主要构造样式是以浅表构造层次的负花状构造及深层剥离断层发育为特征; 断层生长指数、盆地的伸展史和伸展量等参数显示, 晚白垩世是构造转型的重要阶段, 此前主要为走滑构造样式形成阶段, 此后则主要为伸展滑脱构造发育阶段. 在此基础上, 提出松辽盆地具有伸展- 走滑双重力学构造性质, 可能是一个弧后构造盆地.
Persistent Identifierhttp://hdl.handle.net/10722/151100
ISSN
1000-2383
2020 SCImago Journal Rankings: 0.556

 

DC FieldValueLanguage
dc.contributor.authorYan, DPen_US
dc.contributor.authorTian, CLen_US
dc.contributor.authorMeng, LBen_US
dc.contributor.authorZhang, JZen_US
dc.contributor.authorZhou, MFen_US
dc.date.accessioned2012-06-26T06:17:05Z-
dc.date.available2012-06-26T06:17:05Z-
dc.date.issued2003en_US
dc.identifier.citationEarth Science - Journal Of China University Of Geosciences, 2003, v. 28 n. 3, p. 275-280en_US
dc.identifier.citation地球科学 - 中国地质大学学报, 2003, 第28卷 第3期, pp. 275-280-
dc.identifier.issn1000-2383en_US
dc.identifier.urihttp://hdl.handle.net/10722/151100-
dc.description.abstractThe balanced geological sect ion has been widely used for the analysis of orogenic belt, but it is infrequent for ex tensional basins. In this paper, 4 extensional balanced geological sect ion analysis were practiced in Fuyu oil layer of Liangjing , Jilin oilfield, southern Songliao basin with the technology and method, including deformation history restoration, decompaction and erosion restoration. The structure of different ages and the continuous sedimentary sections have been restored. T he result s show that the structural styles possess the characteristics of negative flower structure in the shallow level and ex tensional detachment in deep level. The parameters, including fault growth index, the basin ex tensional history and fault detachment depth, indicate that Late Cretaceous is an important stage for the structure transferring mainly with a strike-slip style before this time and an ex tensional structure and detachment after this time. Therefore, a basin model with twin dynamic property and back-arc characters is proposed.-
dc.description.abstract挤压构造的平衡地质剖面分析已经广泛应用于造山带构造分析, 但伸展构造区的平衡地质剖面分析实例仍然很少. 运用盆地分析的技术与方法, 分层序或阶段将地质构造依次恢复、地层逐层回剥, 并通过在松辽盆地南部吉林两井油田扶余油层4 条剖面的实践, 复原出不同时代盆地构造与地层发育的连续剖面, 揭示出松辽盆地南部主要构造样式是以浅表构造层次的负花状构造及深层剥离断层发育为特征; 断层生长指数、盆地的伸展史和伸展量等参数显示, 晚白垩世是构造转型的重要阶段, 此前主要为走滑构造样式形成阶段, 此后则主要为伸展滑脱构造发育阶段. 在此基础上, 提出松辽盆地具有伸展- 走滑双重力学构造性质, 可能是一个弧后构造盆地.-
dc.languagechien_US
dc.relation.ispartofEarth Science - Journal of China University of Geosciencesen_US
dc.relation.ispartof地球科学 - 中国地质大学学报 (Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao)-
dc.subject平衡地质剖面 (Balanced geological section)-
dc.subject伸展盆地 (Extensional basin)-
dc.subject构造变形史 (Deformational history)-
dc.subject两井油田 (Liangjing oilfield)-
dc.subject松辽盆地 (Songliao basin)-
dc.titleBalanced geological section for extensional tectonic basin and its implication: An example from southern Songliao Basinen_US
dc.title伸展构造盆地的平衡剖面及其构造意义: 以松辽盆地南部为例-
dc.typeArticleen_US
dc.identifier.emailZhou, MF: mfzhou@hkucc.hku.hken_US
dc.identifier.authorityZhou, MF=rp00844en_US
dc.description.naturepublished_or_final_versionen_US
dc.identifier.scopuseid_2-s2.0-0038574944en_US
dc.identifier.hkuros91736-
dc.identifier.volume28en_US
dc.identifier.issue3en_US
dc.identifier.spage275en_US
dc.identifier.scopusauthoridYan, DP=36683417500en_US
dc.identifier.scopusauthoridTian, CL=7102029719en_US
dc.identifier.scopusauthoridMeng, LB=7202236051en_US
dc.identifier.scopusauthoridZhang, JZ=7601354526en_US
dc.identifier.scopusauthoridZhou, MF=7403506005en_US
dc.identifier.issnl1000-2383-

Export via OAI-PMH Interface in XML Formats

OR

Export to Other Non-XML Formats