盆山系统沉积学&mdash;兼论华北和塔里木地区研究实例

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盆山系统沉积学—兼论华北和塔里木地区研究实例

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中图分类号: P512.2 TE121.2

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文章访问数: 1693
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Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

摘要

摘要: 在地球科学领域盆山系统可以作为一种新的地质单元或整体进行研究。在评述国内外研究成果基础上，本文提出了盆山系统分类三原则：即板块构造单元（位置）、盆山形成演化的构造动力学体制、构造—古地理特征或区域源—汇构造—沉积属性，并由此将盆山系统划分为陆内、陆缘（陆洋）和洋内盆山系统三大类及下属十四个亚类。进而论述了盆山系统沉积学的研究体系，其中构造—地层单元与等时地层格架、物源示踪与源汇体系、综合沉积记录及古构造—古气候演变等三方面是研究基础，沉积体系（域）与综合构造—古地理是核心，而盆山演化动力学为学科目标。以华北东部陆内盆山系统为例，研究指出西伯利亚板块与华北—蒙古联合块体的碰撞隆升，形成了该区侏罗纪—早白垩世早期最显著的陆内山—盆系统，而苏鲁造山带碎屑物源影响甚微；以塔里木陆缘盆山系统为例，初步揭示了泥盆—石炭纪西南天山被动陆缘与东南天山弧相关陆缘盆山系统的差异记录。研究认为，为了深化盆山动力学研究，现阶段特别值得在物源示踪与源汇体系、综合沉积记录及古构造—古气候演变方面加强盆山系统沉积学工作。
- 盆山系统 /
- 沉积记录 /
- 源汇体系 /
- 构造&mdash /
- 古地理 /
- 华北块体 /
- 塔里木块体
Abstract: Basin-range system, as a new geological unit or entity, has been accepted and studied in geosciences. Based on reviews on the past research advances, three rules are brought forward for basin-range classification, which includes plate tectonic unit (location), tectonic geodynamical regime, and paleogeographical or tectonic-sedimentary attributes of source-sink systems. There are three basin-range types, intracontinent, continent margin (continent-ocean) and intraocean, and further fourteen sub-typies can be presented in the classification scheme. Then a research frame of basin-range system sedimentology is stated and discussed, in which the tectonic-stratigraphic unit and isochronal stratigraphic framework, provenance tracing and source-sink system, and integrated depositional records and paleotectonic-paleoclimatic evolution are three important research basises; and the depositional system (tract) and integrated tectonic-paleogeography is research core; and the basin-range evolution geodynamics is an subject target of basin-range system sedimentology. As a case study of intracontinent basin-range system in eastern North China, the research shows that the most prominent basin-range system occurred in north North China during Jurassic-early Early Cretaceous due to collision and uplift process between Siberia block and North China-Mongolia one. However, a coexistent source-sink system related to the Su-Lu orogen has weak influences on sedimentary paleogeography of the North China. As another case study of continent margin basin-range system in Tarim area, northwest China, the research basicially reveals differential geological records, reflecting passive and arc-related continent margin basin-range systems, respectively coexisted between west South Tianshan and east one. Finally, in order to deepen the basin-range geodynamics, it is especially suggested to pay attention to academic researches of the provenance tracing and source-sink system and the integrated depositional records and paleotectonic-paleoclimatic evolution.
- basin-range system /
- depositional record /
- source-sink system /
- tectonic-paleogeography /
- North China block /
- Tarim block /

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[1]	许欢, 柳永清, 旷红伟, 彭楠, 丁家翔, 杜研, 苑婷媛. 古风成沉积理论体系与研究进展 . 沉积学报, 2023, 41(6): 1681-1713. doi: 10.14027/j.issn.1000-0550.2023.080
[2]	白亚之, 乔淑卿, 吴斌, 胡利民, 王楠, 范德江, 杨刚, 石学法. 泰国湾百年来有机碳埋藏记录及环境响应 . 沉积学报, 2022, 40(2): 484-493. doi: 10.14027/j.issn.1000-0550.2021.033
[3]	刘晓杰, 季银利, 向荣, 张大海, 李先国. 东海内陆架岩心中木质素的沉积记录 . 沉积学报, 2022, 40(2): 525-533. doi: 10.14027/j.issn.1000-0550.2020.083
[4]	邹灏, 李峤昕, 陈安清, 肖斌, 蒋修未, 黄长成, 胡成辉, 李蝶. 新元古代“雪球地球”形成与消融及华南板块的记录 . 沉积学报, 2022, 40(4): 1043-1058. doi: 10.14027/j.issn.1000-0550.2021.019
[5]	侯云超, 樊太亮, 王宏语, 李一凡, 黄兴文, 龙盛芳. 墨西哥湾西北部古近纪早期（62~48 Ma）源汇体系与沉积格局变迁 . 沉积学报, 2020, 38(6): 1272-1283. doi: 10.14027/j.issn.1000-0550.2019.114
[6]	薛传东, 向坤, 胡廷银, 廖程, 杨欣鹏, 杨天云露, 王磊. 楚雄盆地北部桂花铜矿区晚白垩世含矿岩系沉积环境 . 沉积学报, 2019, 37(3): 491-501. doi: 10.14027/j.issn.1000-0550.2018.153
[7]	罗亮, 王冬兵, 尹福光, 廖世勇, 任飞, 宁括步, 唐渊. 云南保山地块香山组和丁家寨组沉积序列与碳同位素研究 . 沉积学报, 2018, 36(2): 291-301. doi: 10.14027/j.issn.1000-0550.2018.003
[8]	李华, 何幼斌, 黄伟, 刘朱睿鸷, 张锦. 鄂尔多斯盆地南缘奥陶系平凉组深水沉积特征及其与古环境关系——以陕西富平赵老峪地区为例 . 沉积学报, 2018, 36(3): 483-499. doi: 10.14027/j.issn.1000-0550.2018.031
[9]	高抒. 沉积记录研究的现代过程视角 . 沉积学报, 2017, 35(5): 918-925. doi: 10.14027/j.cnki.cjxb.2017.05.005
[10]	. 川北秦岭地区震旦—寒武纪岩相古地理研究新认识 . 沉积学报, 2014, 32(1): 1-7.
[11]	. 青藏高原北部新生代构造演化在柴达木盆地中的沉积记录 . 沉积学报, 2013, 31(05): 824-833.
[12]	. 中国东部陆架全新世沉积体系：过程—产物关系研究进展评述 . 沉积学报, 2013, 31(05): 845-855.
[13]	张哲杜远生毛治超李瑞原小杰. 湘东南桂阳莲塘上泥盆系风暴岩特征及其古地理、古气候意义 . 沉积学报, 2008, 26(3): 369-375.
[14]	朱同兴. 西藏南部聂拉木地区侏罗纪—白垩纪盆—山转换过程中的沉积学响应 . 沉积学报, 2007, 25(2): 293-297.
[15]	曹高社. 华北陆块东南缘凤台组岩相古地理分析 . 沉积学报, 2006, 24(2): 210-216.
[16]	姚书春, 李世杰. 巢湖富营养化过程的沉积记录 . 沉积学报, 2004, 22(2): 343-347.
[17]	林启祥, 王永标, 徐桂荣, 肖诗宇. 东昆仑—阿尼玛卿地区早二叠世的沉积古地理 . 沉积学报, 2001, 19(3): 340-344.
[18]	方国庆, 刘德良, 冯江. 鄂尔多斯盆地早古生代波状构造及其古地理意义 . 沉积学报, 2000, 18(3): 445-448.
[19]	肖传桃, 李维峰, 胡明毅. 江汉盆地早三叠世生态地层学及古地理特征 . 沉积学报, 1997, 15(1): 85-91.
[20]	唐朝晖, 曾允孚. 西秦岭中志留统“硅、灰、泥岩”型层控铀矿的沉积特征及控矿条件 . 沉积学报, 1990, 8(2): 33-42.

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盆山系统沉积学—兼论华北和塔里木地区研究实例

刊出日期: 2013-10-10

中图分类号: P512.2 TE121.2

关键词:

盆山系统 /

沉积记录 /

源汇体系 /

构造— /

古地理 /

华北块体 /

塔里木块体

摘要: 在地球科学领域盆山系统可以作为一种新的地质单元或整体进行研究。在评述国内外研究成果基础上，本文提出了盆山系统分类三原则：即板块构造单元（位置）、盆山形成演化的构造动力学体制、构造—古地理特征或区域源—汇构造—沉积属性，并由此将盆山系统划分为陆内、陆缘（陆洋）和洋内盆山系统三大类及下属十四个亚类。进而论述了盆山系统沉积学的研究体系，其中构造—地层单元与等时地层格架、物源示踪与源汇体系、综合沉积记录及古构造—古气候演变等三方面是研究基础，沉积体系（域）与综合构造—古地理是核心，而盆山演化动力学为学科目标。以华北东部陆内盆山系统为例，研究指出西伯利亚板块与华北—蒙古联合块体的碰撞隆升，形成了该区侏罗纪—早白垩世早期最显著的陆内山—盆系统，而苏鲁造山带碎屑物源影响甚微；以塔里木陆缘盆山系统为例，初步揭示了泥盆—石炭纪西南天山被动陆缘与东南天山弧相关陆缘盆山系统的差异记录。研究认为，为了深化盆山动力学研究，现阶段特别值得在物源示踪与源汇体系、综合沉积记录及古构造—古气候演变方面加强盆山系统沉积学工作。

Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

Publish Date: 2013-10-10

Keywords:

Abstract: Basin-range system, as a new geological unit or entity, has been accepted and studied in geosciences. Based on reviews on the past research advances, three rules are brought forward for basin-range classification, which includes plate tectonic unit (location), tectonic geodynamical regime, and paleogeographical or tectonic-sedimentary attributes of source-sink systems. There are three basin-range types, intracontinent, continent margin (continent-ocean) and intraocean, and further fourteen sub-typies can be presented in the classification scheme. Then a research frame of basin-range system sedimentology is stated and discussed, in which the tectonic-stratigraphic unit and isochronal stratigraphic framework, provenance tracing and source-sink system, and integrated depositional records and paleotectonic-paleoclimatic evolution are three important research basises; and the depositional system (tract) and integrated tectonic-paleogeography is research core; and the basin-range evolution geodynamics is an subject target of basin-range system sedimentology. As a case study of intracontinent basin-range system in eastern North China, the research shows that the most prominent basin-range system occurred in north North China during Jurassic-early Early Cretaceous due to collision and uplift process between Siberia block and North China-Mongolia one. However, a coexistent source-sink system related to the Su-Lu orogen has weak influences on sedimentary paleogeography of the North China. As another case study of continent margin basin-range system in Tarim area, northwest China, the research basicially reveals differential geological records, reflecting passive and arc-related continent margin basin-range systems, respectively coexisted between west South Tianshan and east one. Finally, in order to deepen the basin-range geodynamics, it is especially suggested to pay attention to academic researches of the provenance tracing and source-sink system and the integrated depositional records and paleotectonic-paleoclimatic evolution.

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盆山系统沉积学—兼论华北和塔里木地区研究实例

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Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

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盆山系统沉积学—兼论华北和塔里木地区研究实例

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Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

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盆山系统沉积学—兼论华北和塔里木地区研究实例

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出版历程

Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

计量

出版历程

目录

盆山系统沉积学—兼论华北和塔里木地区研究实例

English Abstract

Basin-Range System Sedimentology and Case Studies in North China and Tarim Areas, China

全文HTML

目录

友情链接

期刊在线

联系我们