秦岭-大别新元古代-中生代沉积盆地演化

张思敏; 姜高磊; 柳坤峰; 王成刚

doi:10.3799/dqkx.2014.103

秦岭-大别新元古代-中生代沉积盆地演化

doi: 10.3799/dqkx.2014.103

张思敏^{1, 2,},
姜高磊^{1, 2},
柳坤峰^{2, 3},
王成刚⁴

1.
中国地质大学地球科学学院，湖北武汉 430074
2.
中国地质大学生物地质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
4.
武汉地质矿产研究所，湖北武汉 430223

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:
张思敏(1990-)，女，硕士研究生，主要从事地层古生物与沉积学研究.E-mail: 979812536@qq.com

中图分类号: P534
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出版历程
- 收稿日期: 2014-04-12
- 刊出日期: 2014-08-01

Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Qinling-Dabie Orogenic Belt

Zhang Simin^{1, 2
,},
Jiang Gaolei^{1, 2},
Liu Kunfeng^{2, 3},
Wang Chenggang⁴

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
4.
Wuhan Institute of Geology and Mineral Resources, Wuhan 430223, China

摘要

摘要: 秦岭-大别造山带处于中央造山带的东部，经历了复杂的构造-沉积历史.在系统分析研究区4个二级和13个三级构造单元岩石地层、化石组合、同位素年代学及构造学等资料的基础上，划分出18个沉积盆地类型，并讨论新元古代-中生代构造-沉积演化：(1)新元古代-早古生代：商丹洋以北的北秦岭为岩浆弧和弧前盆地；南秦岭为陆内裂谷-台盆、台地-陆缘裂谷发育阶段；大别-苏鲁为陆内裂谷-台盆台地发育阶段；(2)晚古生代：北秦岭为海陆交互陆表海；勉略洋于泥盆纪开启；南秦岭为弧后陆棚与台盆台地并存发育阶段；(3)三叠纪：陆陆碰撞造山，全区进入前陆盆地发育阶段；(4)侏罗纪-白垩纪：断陷盆地和压陷盆地发育阶段.
- 秦岭-大别 /
- 新元古代-中生代 /
- 沉积 /
- 构造 /
- 盆地演化
Abstract: As the eastern part of the Central Orogenic Belt, Qinling-Dabie Orogenic Belt has a complicated tectonic-sedimentary history. On the basis of a systematic research on the lithostratigraphy, fossil assemblages, isotopic geochronology and tectonics of 4 secondary and 13 three-level tectonic units, this paper divides the study area into 18 types of sedimentary basins, and discusses its tectonic-sedimentary evolution from Neoproterozoic to Mesozoic: (1) Neoproterozoic-Early Paleozoic: North Qinling was magmatic arc and forearc basin; South Qinling experienced intracontinental rift to interplatform basin-platform to continental-margin rift; Dabie-Sulu experienced intracontinental rift to interplatform basin-platform. (2) Late Paleozoic: North Qinling was marine-continental alternation epeiric sea; Mianlüe oceanic basin opened in the Devonian; South Qinling was backarc shelf and interplatform basin-platform at the same time. (3)Triassic: continental collision orogeny, stage of foreland basins. (4) Jurassic-Cretaceous: stage of fault basins and depressional basins.
- Qinling-Dabie /
- Neoproterozoic-Mesozoic /
- sedimentology /
- tectonics /
- basin evloution

HTML全文

图 1 秦岭-大别造山带大地构造格局与构造单元划分

Ⅰ.宽坪-佛子岭对接带，Ⅰ-1.宽坪俯冲增生杂岩带，Ⅰ-2.淮阳-佛子岭增生杂岩带，Ⅰ-3.斜峪关-二郎坪岛弧；Ⅱ.秦岭弧盆系，Ⅱ-1.北秦岭(太白-商州)地块，Ⅱ-2.商丹蛇绿混杂岩，Ⅱ-3.南秦岭陆缘盆地，Ⅱ-4.泽库前陆盆地，Ⅱ-5.西倾山-南秦岭陆缘裂谷，Ⅱ-6.勉略蛇绿混杂岩；Ⅲ.大别-苏鲁地块，Ⅲ-1.大别地块，Ⅲ-2.苏鲁地块；Ⅳ.武当-随南陆缘裂谷，Ⅳ-1.武当-随州陆内裂谷，Ⅳ-2.南襄断陷盆地；据潘桂棠等，2009

Fig. 1. Qinling-Dabie orogenic belt tectonic framework and tectonic units

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图 2 宽坪-佛子岭沉积演化柱状图

K₁j.鸡山组；K₁z.周家湾组；K₁t.田家坝组；K₁c.陈棚组；J₁s.三尖铺组；J₃f.凤凰台组；J₃z.周公山组；T₃tz.太子山组；T₃t.太山庙组；T₃w.五里川组；Pz₁h.火神庙组；Pz₁l.刘山崖组；C₂y.杨小庄组；C₂h.胡油坊组；C₂d.道人冲组；C₁y.杨山组；C₁h.花园墙组

Fig. 2. Column of the sedimentary evolution of Kuanping-Foziling

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图 3 北秦岭、商丹、南秦岭地层分区沉积演化柱状图

Fig. 3. Column of the sedimentary evolution of North Qinling, Shangdan and South Qinling area

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图 4 泽库、西倾山-南秦岭、勉略地层分区沉积演化柱状图

K₁mg.蘑菇山组；K₁D.东河群；T₃y.两河口组；T₃l.雅江组；T₃x.新都桥组；T₃r.如年各组；T₃zh.侏倭组；T₃d.大河坝组；T_2-3g.光盖山组；T₁j.江里沟组；T₁m.马热松多组；T₁z.扎里山组；O_2-3gj.干江河组

Fig. 4. Column of the sedimentary evolution of Zeku, Xiqingshan-South Qinling and Mianlue area

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图 5 大别、苏鲁、武当-随州、南襄地层分区沉积演化柱状图

K₂jz.胶州组；K₂j.金岗口组；K₂h.红土崖组；K₂x.辛格庄组；K₂l.林家庄组；K₁f.法家茔组；K₁m.马连坡组；K₁d.杜村组；K₁qg.曲格庄组；K₁c.城山后组；K₁y.杨家庄组；K₁s.水南组；K₁l.龙旺庄组；K₁z.止凤庄组；K₁ls.林寺山组；K₁w.瓦屋夼组

Fig. 5. Column of the sedimentary evolution of Dabie, Sulu, Wudang-Suizhou and Nanxiang area

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图 6 秦岭-大别构造演化示意

Fig. 6. Sketch map of the tectonic evolution of Qinling-Dabie

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