ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
陆相断陷盆地二级层序时限构造沉降与湖平面变化的响应关系
  
关键词:continental rift basin  tectonic subsidence  sequence stratigraphy  lake-level variation
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王家豪 中国地质大学资源学院, 湖北武汉 430074中国地质大学构造与油气资源教育部重点实验室, 湖北武汉 430074 cugwangjiahao@163.com 
王华 中国地质大学资源学院, 湖北武汉 430074  
廖远涛 中国地质大学资源学院, 湖北武汉 430074  
肖敦清 中国石油天然气总公司中石油大港油田分公司勘探开发研究院, 天津 300280  
尚亚乐 中国地质大学资源学院, 湖北武汉 430074  
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摘要:
Lake-level Variation Response to Tectonic Subsidence in a Second-Order Sequence of Continental Rift Basin
      To pursue the lake-level variation response to tectonic subsidence in the continental rift basin, this paper introduced two parameters (subsidence flux and subsidence velocity flux) to show the whole characteristics of basement subsidence by using two-dimensional stripping-back analysis. In the Dongying Formation of the middle Huanghua depression, the delta depositional system is well developed. The Dongying Formation, as a second-order sequence, can be subdivided into four third-order sequences. Tectonic subsidence gradually weakened and subse-quently strengthened during the development of the Dongying Formation, characterized by intense rift faulting followed by later increasing down-warping. Combined with tectonic subsidence, depositional evolution and se-quence framework of the Dongying Formation, this paper holds that the fall of the lake-level and the flourishing of the delta depositional system were coupled with rapid tectonic subsidence, and the lake-level fall resulted from violent unbalanced tectonic subsidence, causing redistribution of lake-water towards main faults or down-warping centers. The lake-water supplement was insufficient compared with the newly increased accommodation space due to tectonic subsidence. As a result, the rise of the lake-level and the development of the deep lake corresponded to slow tectonic subsidence, and the lake-level variation had nothing to do with the gross of tectonic subsidence
WANG Jia-hao,WANG Hua,LIAO Yuan-tao,XIAO Dun-qing,SHANG Ya-le.2009.Lake-level Variation Response to Tectonic Subsidence in a Second-Order Sequence of Continental Rift Basin[J].Acta Geoscientica Sinica,30(2):194-200.
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