苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

傅  强

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苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

傅强

文章导航 > 沉积学报 > 2007 > 25(3): 380-385

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

引用本文:

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

Citation:

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

引用本文:

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

Citation:

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

傅强

同济大学海洋地质国家重点实验室上海 200092

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通讯作者:
傅强

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文章访问数: 1976
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Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

FU Qiang

State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

More Information

Corresponding author: FU Qiang

摘要

摘要: 通过对苏北盆地钻井岩心分析研究总结得出，在晚白垩世、古新世苏北盆地曾与海相通，并遭受海侵影响。海侵的原因，可能是从晚白垩世晚期起，中国东部的地应力条件以引张力占优势，并在华北—渤海湾、苏北—南黄海和东海陆架区，发育了一系列为早第三纪巨厚沉积物所充填的半地堑箕状盆地，海水由东海向黄海海侵，造成陆架上箕状盆地在短时期内与海水相通。苏北盆地在晚白垩世泰州组—古新世阜宁组沉积形成了以全盆地阜二段、阜四段为主，局部泰二段的富含介形虫的暗色泥岩，成为该盆地的主力烃源岩。古生物以及岩矿、地球化学等方面的证据可以确定苏北盆地晚白垩世—古新世发育的湖盆环境可统称“近海湖泊”或将海侵层段称“海侵湖泊”，而至始新世戴南和三垛组沉积时则可统称内陆湖泊和河流冲积平原环境。通过对苏北盆地晚白垩世—古新世海侵湖泊的确切与充分的认识分析，不仅对苏北盆地晚白垩世—古新世时期的湖盆古地理重建，而且对烃源岩的发育与分布以及生油气潜力评价都具有重要的意义。
- 苏北盆地 /
- 晚白垩世—古新世 /
- 海侵 /
- 湖泊
Abstract: Based on the analysis of core of Subei basin during late Cretaceous and Paleocene Epoch, the authors conclude that Subei Basin was linked with the sea and the deposit was affected by transgression. The causes of marine transgression may be the tension power have predominated the groundstress condition of the east China and develop a series of halfgrabenlike basin which was filled by huge thick sediment of early Tertiary in shelf of HuabeiBohai gulf , Subeisouth yellow sea and East China sea. Consequently, seawater transgresses from East China Sea to yellow sea and connects half grabenlike basin on the shelf and sea during short period. During the sediment of late Cretaceous Taizhou Formation and Paleocene Epoch Funing Formation, Subei Basin have formed dark shale containing lots of ostracoda that include predominated whole basin E1f2 Formation and E1f4 Formation and local K2t2 Formation, which have become main source rocks of the basin. The evidences of paleontology, minerals in rocks and geochemistry can ascertain the environment of lake basin which develops during late Cretaceous and Paleocene Epoch. This environment was generally designated "near sea lake basin" or the layer and member that was transgressed by sea was called "transgression lake basin", whereas, which was generally called inland lake and river alluvium plain during sediment of Eocene Dainan Formation and Sanduo Formation. Based on the analysis and sufficiency cognition of Transgression Lake of late Cretaceous and Paleocene Epoch of Subei Basin, the research is important to not only paleogeographic reconstruction of Subei basin during late Cretaceous and Paleocene Epoch but also the comment to make upon development and distribution of the source rocks and potential of oil and gas generation.
- Subei Basin /
- late Cretaceous and Paleocene Epoch /
- transgression lake /

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[1]	刘建宁, 董桂玉, 王兵杰, 张琳婷, 霍少川, 曹玉鹏, 彭凯, 冷春鹏. 苏北盆地高邮凹陷戴南组震积岩特征及其石油地质意义 . 沉积学报, 2018, 36(6): 1267-1276. doi: 10.14027/j.issn.1000-0550.2018.095
[2]	李维, 朱筱敏, 陈刚, 马英俊. 基于等时界面识别的浅水三角洲-河流沉积体系研究——以高邮凹陷黄珏地区古近系垛一段为例 . 沉积学报, 2018, 36(1): 110-119. doi: 10.3969/j.issn.1000-0550.2018.013
[3]	张慧芳, 吴欣松, 王斌, 段云江, 屈洋, 陈德飞. 陆相湖盆沉积有机质富集机理研究进展 . 沉积学报, 2016, 34(3): 463-477. doi: 10.14027/j.cnki.cjxb.2016.03.004
[4]	刚文哲. 高邮凹陷真武油田成藏期与动态成藏过程分析 . 沉积学报, 2011, 29(3): 580-586.
[5]	柳蓉. 抚顺盆地始新世古湖泊演化 . 沉积学报, 2010, 28(4): 688-695.
[6]	周健. 苏北盆地高邮凹陷马家嘴地区古近系戴南组物源分析 . 沉积学报, 2010, 28(6): 1117-1128.
[7]	舒强. 苏北盆地浅钻沉积物磁化率与粒度记录的末次冰消期以来的环境变化 . 沉积学报, 2009, 27(1): 111-117.
[8]	张功成. 珠江口盆地—琼东南盆地深水区古近系沉积演化 . 沉积学报, 2009, 27(4): 632-641.
[9]	樊馥. 孙吴—嘉荫盆地太平林场组烃源岩海侵特征研究 . 沉积学报, 2009, 27(4): 650-656.
[10]	杨永才. 溱潼凹陷红庄油田凝析油的油源及成藏期 . 沉积学报, 2008, 26(3): 531-539.
[11]	舒强. 苏北盆地XH1＃钻孔沉积物磁化率与粒度组分相关性变化特征及其意义研究 . 沉积学报, 2006, 24(2): 276-281.
[12]	. 海侵背景下风暴控制的滨岸—陆棚砂体研究——以塔中志留系下沥青砂岩段为例 . 沉积学报, 2006, 24(4): 468-475.
[13]	张喜林. 苏北盆地高邮凹陷古近系戴南组滨浅湖沉积中的遗迹化石 . 沉积学报, 2006, 24(1): 81-89.
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苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

傅强

同济大学海洋地质国家重点实验室上海 200092

通讯作者: 傅强

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-06-10

关键词:

苏北盆地 /

晚白垩世—古新世 /

海侵 /

湖泊

摘要: 通过对苏北盆地钻井岩心分析研究总结得出，在晚白垩世、古新世苏北盆地曾与海相通，并遭受海侵影响。海侵的原因，可能是从晚白垩世晚期起，中国东部的地应力条件以引张力占优势，并在华北—渤海湾、苏北—南黄海和东海陆架区，发育了一系列为早第三纪巨厚沉积物所充填的半地堑箕状盆地，海水由东海向黄海海侵，造成陆架上箕状盆地在短时期内与海水相通。苏北盆地在晚白垩世泰州组—古新世阜宁组沉积形成了以全盆地阜二段、阜四段为主，局部泰二段的富含介形虫的暗色泥岩，成为该盆地的主力烃源岩。古生物以及岩矿、地球化学等方面的证据可以确定苏北盆地晚白垩世—古新世发育的湖盆环境可统称“近海湖泊”或将海侵层段称“海侵湖泊”，而至始新世戴南和三垛组沉积时则可统称内陆湖泊和河流冲积平原环境。通过对苏北盆地晚白垩世—古新世海侵湖泊的确切与充分的认识分析，不仅对苏北盆地晚白垩世—古新世时期的湖盆古地理重建，而且对烃源岩的发育与分布以及生油气潜力评价都具有重要的意义。

English Abstract

Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

FU Qiang

State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

Corresponding author: FU Qiang

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2007-06-10

Keywords:

Abstract: Based on the analysis of core of Subei basin during late Cretaceous and Paleocene Epoch, the authors conclude that Subei Basin was linked with the sea and the deposit was affected by transgression. The causes of marine transgression may be the tension power have predominated the groundstress condition of the east China and develop a series of halfgrabenlike basin which was filled by huge thick sediment of early Tertiary in shelf of HuabeiBohai gulf , Subeisouth yellow sea and East China sea. Consequently, seawater transgresses from East China Sea to yellow sea and connects half grabenlike basin on the shelf and sea during short period. During the sediment of late Cretaceous Taizhou Formation and Paleocene Epoch Funing Formation, Subei Basin have formed dark shale containing lots of ostracoda that include predominated whole basin E1f2 Formation and E1f4 Formation and local K2t2 Formation, which have become main source rocks of the basin. The evidences of paleontology, minerals in rocks and geochemistry can ascertain the environment of lake basin which develops during late Cretaceous and Paleocene Epoch. This environment was generally designated "near sea lake basin" or the layer and member that was transgressed by sea was called "transgression lake basin", whereas, which was generally called inland lake and river alluvium plain during sediment of Eocene Dainan Formation and Sanduo Formation. Based on the analysis and sufficiency cognition of Transgression Lake of late Cretaceous and Paleocene Epoch of Subei Basin, the research is important to not only paleogeographic reconstruction of Subei basin during late Cretaceous and Paleocene Epoch but also the comment to make upon development and distribution of the source rocks and potential of oil and gas generation.

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

引用本文:

傅强. 苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义[J]. 沉积学报, 2007, 25(3): 380-385.

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

Citation:

FU Qiang. Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance[J]. Acta Sedimentologica Sinica, 2007, 25(3): 380-385.

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苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

通讯作者:
傅强

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Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

Corresponding author: FU Qiang

计量

目录

苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

同济大学海洋地质国家重点实验室上海 200092

通讯作者: 傅强

English Abstract

Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

Corresponding author: FU Qiang

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苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

通讯作者: 傅 强

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Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

Corresponding author: FU Qiang

计量

出版历程

目录

苏北盆地晚白垩世—古新世海侵湖泊的证据及其地质意义

同济大学海洋地质国家重点实验室 上海 200092

通讯作者: 傅 强

English Abstract

Evidence of Transgression Lake of Subei Basin During Late Cretaceous and Paleocene Epoch and Its Geological Significance

State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092

Corresponding author: FU Qiang

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期刊在线

联系我们

通讯作者:
傅强

同济大学海洋地质国家重点实验室上海 200092

通讯作者: 傅强