华北陆块新元古代-中生代沉积盆地划分及其构造演化

郝奕玮; 骆满生; 徐增连; 邹亚锐; 唐婷婷

doi:10.3799/dqkx.2014.106

华北陆块新元古代-中生代沉积盆地划分及其构造演化

doi: 10.3799/dqkx.2014.106

郝奕玮^{1, 2,},
骆满生^2, ,,
徐增连^{1, 2},
邹亚锐^{1, 3},
唐婷婷^{1, 3}

1.
中国地质大学地球科学学院，湖北武汉 430074
2.
中国地质大学生物与环境地质国家重点实验室，湖北武汉 430074
3.
中国地质大学地质调查研究院，湖北武汉 430074

基金项目:

中国地质调查局项目 1212010733802

中国地质调查局项目 12120113012500

详细信息

作者简介:
郝奕玮(1990-)，女，硕士，主要从事地层古生物和沉积学研究.E-mail: 553171281@qq.com

通讯作者:
骆满生，E-mail: 937830430@qq.com

中图分类号: P534
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- 被引次数: 0
出版历程
- 收稿日期: 2013-05-28
- 刊出日期: 2014-08-01

Division of Sedimentary Basins and Its Tectonic Evolution in North China from Newproterozoic to Mesozoic

Hao Yiwei^{1, 2
,},
Luo Mansheng^{2
, ,},
Xu Zenglian^{1, 2},
Zou Yarui^{1, 3},
Tang Tingting^{1, 3}

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 在华北陆块区进行构造-地层区划的基础上，对华北陆块中元古代-新元古代、早古生代、晚古生代、三叠纪-早侏罗世、中侏罗世-白垩纪5个大地构造阶段不同构造-地层区内的沉积盆地类型、充填序列和时空演化过程进行了分析、讨论.中-新元古代是华北周缘裂谷发育期.寒武纪-早、中奥陶世，华北广泛发生沉降并接受海侵，形成几乎广布全华北的碳酸盐岩台地.晚奥陶世-泥盆纪，华北整体抬升，遭受剥蚀，沉积缺失.石炭纪-二叠纪，华北陆块再次发生沉降并接受海侵，形成广阔的陆表海海陆交互相沉积，至晚二叠世华北陆块进入陆相盆地发展阶段.中生代，华北陆块陆内构造运动活跃，普遍形成与火山活动相伴的断陷盆地、坳陷盆地和拉分盆地.
- 沉积 /
- 构造 /
- 盆地演化 /
- 新元古代-中生代 /
- 华北陆块
Abstract: On the basis of divisions of tectonic-stratum of the North China block (NCB) area, this article discusses the type of sedimentary basins formation region, filling sequence and temporal evolution of different tectonic-stratum zones for each construction phase according to five tectonic stages as Mesoproterozoic-Neoproterozoic, Paleozoic, Late Paleozoic, Triassic-Early Jurassic, Middle Jurassic-Cretaceous. Meso-Neoproterozoic is the stage of development of periphery rifting. Cambrian-Early, Middle Ordovician, North China plate synchronized global settlement and received extensive transgression, forming widespread carbonate platform of almost all north China. Late Ordovician-Devonian, NCB overall uplift and erosion, sedimentation is missing. Carboniferous-Permian, North China block subsided again and suffered transgression, forming a broad epicontinental sea paralic deposition. To Late Permian, NCB entered the stage of continental basin development. Mesozoic, continental tectonic activities were active, forming fault basins, sag basins and pull-apart basins broadly.
- sedimentology /
- tectonics /
- Neoproterozoic-Mesozoic /
- North China /

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图 1 华北构造分区

Ⅰ.冀北-阴山(陆块)地层区；Ⅱ.鄂尔多斯(陆块)地层区；Ⅲ.五台-太行地层区；Ⅳ.冀辽陆块地层区；Ⅴ.渤海东(陆块)地层区；Ⅵ.鲁西(陆块)地层区；Ⅶ.陕豫皖(陆块)地层区；1.Ⅵ-1-1狼山地层分区；2.Ⅵ-1-2色尔腾地层分区；3.Ⅵ-1-3红旗营子、冀北地层分区；4.Ⅵ-2-1吉兰泰-包头地层分区；5.Ⅵ-2-2乌拉山-凉城地层分区；6.Ⅵ-2-3贺兰山地层分区；7.Ⅵ-2-4鄂尔多斯地层分区；8.Ⅵ-3-1山西地层分区；9.Ⅵ-3-2恒山-桑干地层分区；10.Ⅵ-3-3太行山北段地层分区；11.Ⅵ-3-4五台-吕梁地层分区；12.Ⅵ-3-5汾渭地层分区；13.Ⅵ-3-6阜平地层分区；14.Ⅵ-3-7沁水地层分区；15.Ⅵ-3-8赞皇-涑水地层分区；16.Ⅵ-4-1承德-建平地层分区；17.Ⅵ-4-2凡河地层分区；18.Ⅵ-4-3燕辽地层分区；19.Ⅵ-4-4绥中-秦皇岛地层分区；20.Ⅵ-4-5冀东地层分区；21.Ⅵ-4-6遵化地层分区；22.Ⅵ-4-7渤海地层分区；23.Ⅵ-4-8下辽河地层分区；24.Ⅵ-5-1龙岗地层分区；25.Ⅵ-5-2太子河-浑江地层分区；26.Ⅵ-5-3胶-辽-吉地层分区；27.Ⅵ-5-4大连地层分区；28.Ⅵ-5-5胶东地层分区；29.Ⅵ-5-6招远地层分区；30.Ⅵ-5-7莱阳地层分区；31.Ⅵ-6-1泰山地层分区；32.Ⅵ-6-2鲁西地层分区；33.Ⅵ-6-3淄博(枣庄)地层分区；34.Ⅵ-7-1中条-登封地层分区；35.Ⅵ-7-2熊耳、太华-鲁山地层分区；据潘桂棠等(2009)修改

Fig. 1. Tectonic division of North China

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图 2 华北陆块新元古代各构造阶段沉积盆地分布及地层格架

1.狼山隆起；2.贺兰山-鄂尔多斯混积台地(Qb)；3.色尔腾裂谷(Qb)；4.乌拉山-凉城碳酸盐岩台地(Z2)；5.冀北隆起；6.恒山-桑干、五台-吕梁隆起；7.汾渭、沁水隆起；8.赞皇-涑水隆起；9.山西碎屑岩陆表海(Qb)；10.太行山北段混积台地(Qb)；11.燕辽混积台地(Qb)；12.渤海混积台地(Qb)；13.下辽河隆起；14.凡河裂谷(Qb)；15.张广才岭-长白山被动陆缘(Qb-Z)；16.大连-泰山隆起；17.鲁西碳酸盐岩台地(Qb-Z1)；18.中条-登封被动陆缘(Z)；19.太华-鲁山裂谷(Qb)

Fig. 2. Division of Neoproterozoic sedimentary basin of North China and stratigraphic framework

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图 3 华北陆块新元古代－早古生代各构造阶段沉积盆地分布图及地层格架

1.狼山隆起；2.阴山被动陆缘(Z-O)；3.贺兰山混积台地()；4.华北碳酸盐岩台地()；5.辽东隆起；6.胶东隆起；7.熊耳-鲁山被动陆缘；O_1-2m.马家沟组；O_1-2b.米钵山组；O₃sh.山子沟组；O₃y.银川组；O₁sh.水泉岭组；O₂s.三道沟组；O₂p.平凉组；O₃j.姜家湾组

Fig. 3. Division of Early Paleozoic sedimentary basin of North China and stratigraphic framework

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图 4 华北陆块晚古生代－早侏罗世各构造阶段沉积盆地分布图及地层格架

a.晚古生代-早中三叠世；其中，1.阴山隆起；2.贺兰山海陆交互陆表海(C₂-P₂)、前陆盆地(P₂-T)；3.吕梁山海陆交互陆表海(C₂-P₂)、坳陷盆地(P₂-T)；4.汾渭-沁水海陆交互陆表海；5.太行山北段、渤海隆起；6.泰山-淄博海陆交互陆表海(C₂-P₂)、坳陷盆地(P₂-T)；7.太子河-浑江、胶-辽-吉海陆交互陆表海(C₂-P₂)、坳陷盆地(P₂-T₂)；8.燕辽海陆交互陆表海(C₂-P₂)、坳陷盆地(P₂-T)；9.承德-凡河隆起；10.下辽河隆起；11.龙岗海陆交互陆表海(C₂-P₁)；12.中条-登封海陆交互陆表海(C₂-P₂)、坳陷盆地(P_2-3)；13.熊耳-鲁山隆起；14.冀东隆起；15.大连隆起；b.晚三叠世-早侏罗世；其中，1.狼山-色尔腾压陷盆地(J₁-K₁)；2.吉兰泰-包头隆起；3.贺兰山-鄂尔多斯前陆盆地(C₂-P₂)、压陷盆地(P₂-T)；4.大青山弧内裂陷盆地(J₁-J₃)；5.遵化隆起；6.燕辽坳陷盆地(P₂-T)、压陷盆地(J₁)；7.绥中-秦皇岛压陷盆地(J₁)；8.凡河压陷盆地(J₁)；9.山西前陆盆地(T₁)、弧内裂陷盆地(J)；10.汾渭、沁水前陆盆地(T)；11.五台-吕梁坳陷盆地(P₂-T)、断陷盆地(J)；12.阜平-涑水隆起；13.渤海隆起；14.下辽河隆起；15.龙岗弧内裂陷盆地(J₁-K₂)；16.胶-辽-吉弧内裂陷盆地(T₃-K₁)；17.太子河-浑江坳陷盆地(P₂-T₂)、(火山)断陷盆地(J₁-K₂)；18.中条-登封前陆盆地(T)、压陷盆地(J)；19.熊耳-鲁山隆起

Fig. 4. Division map of Late Paleozoic-Early Jurassic sedimentary basin of North China and stratigraphic framework

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图 5 华北陆块中侏罗世-晚白垩世各构造阶段沉积盆地分布图及地层格架

1.狼山压陷盆地(J₁-K₁)，(火山)断陷盆地(K₁)；2.贺兰山压陷盆地(J₁-K₁)；3.冀北弧内裂陷盆地(J)，(火山)断陷盆地(K)；4.恒山-桑干弧内裂陷盆地(J₂-K₁)，坳陷盆地(K₂)；5.山西弧内裂陷盆地(J)，断陷盆地(K)；6.五台-吕梁断陷盆地(J)；7.沁水断陷盆地(J₃)；8.汾渭隆起；9.阜平-涑水隆起；10.渤海(火山)断陷盆地(J₃)；11.招远-莱阳(火山)拉分盆地(K)；12.大青山弧内裂陷盆地(J₁-K₂)；13.燕辽断陷盆地(J_2-3)，弧内裂陷盆地(K)；14.下辽河拉分盆地(K₁)；15.龙岗弧内裂陷盆地(J₁-K₂)；16.太子河-浑江(火山)断陷盆地(J₁-K₂)；17.胶-辽-吉弧内裂陷盆地(J₃-K₁)，坳陷盆地(K₂)；18.大连断陷盆地(J₂)；19.胶东断陷盆地(K₁)；20.鲁西拉分盆地(J₂-K₂)；21.中条-登封压陷盆地(J)，(火山)断陷盆地(K)；22.熊耳-鲁山断陷盆地(K₂)

Fig. 5. Division map of Middle Jurassic-Late Cretaceous sedimentary basin of North China and stratigraphic framework

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图 6 华北地区新元古代-中生代沉积盆地构造演化

(据刘波等，1999修改)

Fig. 6. The tectonic evolution chart of Neoproterozoic-Mesozoic sedimentary basin at North China

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