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青藏高原羌塘古生界研究进展与存在问题
Research progress and existing issues on the paleozoic strata in the Qiangtang Terrane of the Qinghai-Xizang Plateau
- 西北大学学报（自然科学版） 2025年55卷第3期 页码：501-522
- 作者机构：
1.吉林大学地球科学学院，吉林 长春 130061
2.吉林大学青藏高原地质研究中心，吉林 长春 130061
3.自然资源部东北亚矿产资源评价重点实验室，吉林 长春 130061
4.中国地质调查局西安地质调查中心〔西北地质科技创新中心〕，陕西 西安 710119
- 作者简介：
[ "解超明，博士，吉林大学教授，博士生导师，入选自然资源部高层次科技创新人才工程（地质找矿方向）青年科技人才，主要从事青藏高原特提斯构造演化研究。主持国家自然科学基金项目3项，以第一/通讯作者发表SCI论文35篇，出版学术专著1部。担任《沉积与特提斯地质》编委及Journal of Earth Science、《西北大学学报（自然科学版）》《地质通报》《地球科学》等期刊青年编委。曾获得自然资源科学技术奖（科技进步奖）一等奖（R3）、青藏高原青年科技奖、吉林大学李四光优秀青年教师奖等。" ]
- 基金信息：国家自然科学基金(41872231;42172226)
DOI：10.16152/j.cnki.xdxbzr.2025-03-003
中图分类号： P56收稿日期：2025-03-30，
纸质出版日期：2025-06-25
- 稿件说明：
移动端阅览
解超明, 史哲, 段梦龙, 等. 青藏高原羌塘古生界研究进展与存在问题[J]. 西北大学学报（自然科学版）, 2025,55(3):501-522.
XIE Chaoming, SHI Zhe, DUAN Menglong, et al. Research progress and existing issues on the paleozoic strata in the Qiangtang Terrane of the Qinghai-Xizang Plateau[J]. Journal of northwest university (natural science edition), 2025, 55(3): 501-522.
解超明, 史哲, 段梦龙, 等. 青藏高原羌塘古生界研究进展与存在问题[J]. 西北大学学报（自然科学版）, 2025,55(3):501-522. DOI： 10.16152/j.cnki.xdxbzr.2025-03-003.
XIE Chaoming, SHI Zhe, DUAN Menglong, et al. Research progress and existing issues on the paleozoic strata in the Qiangtang Terrane of the Qinghai-Xizang Plateau[J]. Journal of northwest university (natural science edition), 2025, 55(3): 501-522. DOI： 10.16152/j.cnki.xdxbzr.2025-03-003.
摘要
羌塘处于青藏高原腹地，在大地构造上以龙木错—双湖缝合带（羌塘中央隆起带）为界划分为羌南和羌北两个地块。羌塘中部的蛇绿混杂岩、高压变质岩以及弧岩浆岩等方面的大量前期研究表明，龙木错—双湖古特提斯洋至少从寒武纪打开、持续或阶段性演化到三叠纪，使得羌南和羌北在古生代期间分属于冈瓦纳与劳亚大陆体系。在综述前人研究基础上，系统总结了羌塘中央隆起带古生界的物质组成、时空分布特征以及地层的划分与对比情况。通过梳理研究发现，羌南和羌北的古生界沉积记录相对完整和连续，但研究程度仍明显偏低，南、北羌塘古生代盆地充填与演化研究明显不足，有关龙木错—双湖古特提斯洋及两侧大陆边缘的演化历史并不清楚，羌塘盆地结构与构造属性与羌塘油气远景评价等基础地质工作亟须开展。开展羌塘古生界研究，不仅能有效揭示古特提斯洋的演化历史，对重塑古特提斯洋-陆构造格局具有重要约束意义，同时，对认识羌塘盆地基底性质与结构、进行羌塘油气资源调查等具有重要的实践指导意义。
Abstract
The Qiangtang region
situated in the hinterland of the Qinghai-Xizang Plateau
is tectonically divided into the South Qiangtang and North Qiangtang Terranes by the Longmu Co-Shuanghu Suture Zone (Central Qiangtang Uplift Zone). Previous studies
based on extensive investigations of ophiolitic mélanges
highpressure metamorphic rocks
and arc magmatic rocks
have demonstrated that the Paleo-Tethys Ocean in the Longmu Co-Shuanghu area opened at least during the Cambrian and evolved continuously or episodically until the Triassic. This tectonic evolution resulted in the separation of South and North Qiangtang into the Gondwana and Laurasia continental systems
respectively
during the Paleozoic. Building upon a synthesis of prior research
this research systematically summarizes the material composition
spatiotemporal distribution characteristics
and stratigraphic division and correlation of the Paleozoic sequences in the Central Qiangtang Uplift Zone. The review reveals that the Paleozoic sedimentary records in both South and North Qiangtang are relatively complete and continuous. However
the current level of research remains notably insufficient. Critical gaps persist in understanding the Paleozoic basin fill
evolutionary processes
and the tectonic history of the Longmu Co-Shuanghu Paleo-Tethys Ocean and its associated continental margins. Fundamental geological investigations-such as clarifying the basin architecture
tectonic attributes
and petroleum potential evaluation of the Qiangtang Basin are urgently required. This research contends that advancing research on the Qiangtang Paleozoic sequences will not only elucidate the evolutionary history of the Paleo-Tethys Ocean
but also provide critical constraints for reconstructing the ocean-continent tectonic framework of the Paleo-Tethyan regime. Furthermore
it holds significant practical implications for deciphering the basement properties and architecture of the Qiangtang Basin and guiding future hydrocarbon exploration in the region.
关键词
Keywords
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