二连盆地乌尼特坳陷早白垩世构造特征——深部构造与浅部构造的关联

苗全芸, 漆家福, 肖阳, 范绳, 魏秀丽. 二连盆地乌尼特坳陷早白垩世构造特征——深部构造与浅部构造的关联[J]. 地质科学, 2015, 50(2): 553-563. doi: 10.3969/j.issn.0563-5020.2015.013
引用本文: 苗全芸, 漆家福, 肖阳, 范绳, 魏秀丽. 二连盆地乌尼特坳陷早白垩世构造特征——深部构造与浅部构造的关联[J]. 地质科学, 2015, 50(2): 553-563. doi: 10.3969/j.issn.0563-5020.2015.013
Miao Quanyun, Qi Jiafu, Xiao Yang, Fan Sheng, Wei Xiuli. Early Cretaceous structural feature of the Wunite depression in Erlian Basin: A connection between deep-level and shallow-level structures[J]. Chinese Journal of Geology, 2015, 50(2): 553-563. doi: 10.3969/j.issn.0563-5020.2015.013
Citation: Miao Quanyun, Qi Jiafu, Xiao Yang, Fan Sheng, Wei Xiuli. Early Cretaceous structural feature of the Wunite depression in Erlian Basin: A connection between deep-level and shallow-level structures[J]. Chinese Journal of Geology, 2015, 50(2): 553-563. doi: 10.3969/j.issn.0563-5020.2015.013

二连盆地乌尼特坳陷早白垩世构造特征——深部构造与浅部构造的关联

详细信息
    作者简介:

    苗全芸,女,1987年9月生,博士研究生,石油地质学和构造地质学专业。E-mail:mqycup@163.com

  • 中图分类号: P54

Early Cretaceous structural feature of the Wunite depression in Erlian Basin: A connection between deep-level and shallow-level structures

  • 乌尼特坳陷属于二连盆地五大坳陷之一, 内部发育一系列地堑、半地堑, 主要充填地层为下白垩统。坳陷基底由晚古生代复式向斜及二连—贺根山混杂岩带(Pz2)组成。乌尼特坳陷早白垩世断陷结构和分布组合与基底构造紧密相关。复式向斜断陷带基底为北东向、北北东向晚古生代复式向斜, 受基底控制早白垩世发育一系列北东向、北北东向断陷。断陷带北部主干断层向深部延伸时受复式向斜构造层韧性伸展变形影响而在浅层滑脱, 形成浅而宽阔的断陷, 主要为并联式组合。断陷带南部终止于混杂岩带并与之斜交, 主干断层向深部延伸时受混杂岩带伸展走滑构造变形影响而在浅层滑脱, 形成浅而狭长的断陷, 主要为斜列式组合。二连—贺根山混杂岩断陷带基底为混杂岩带, 受基底控制早白垩世发育一系列北东向、北北东向断陷。断陷主干断层向深部延伸时受以伸展为主的构造变形影响而在混杂岩深层滑脱, 形成深而狭长的断陷, 以串联或并联式组合。
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出版历程
收稿日期:  2014-09-10
修回日期:  2015-01-06
刊出日期:  2015-04-25

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