浙西北地区上奥陶统物源及古地理意义：来自沉积学、碎屑组成及年代学的证据

于涛; 王宗起; 王东升; 刘宣妤; 马收先; 聂潇; 马昌前

doi:10.3799/dqkx.2022.410

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3649-3670

Yu Tao, Wang Zongqi, Wang Dongsheng, Liu Xuanyu, Ma Shouxian, Nie Xiao, Ma Changqian, 2023. Provenance and Paleogeographic Significance of Upper Ordovician in NW Zhejiang: Evidence from Sedimentology, Clastic Composition and Chronology. Earth Science, 48(10): 3649-3670. doi: 10.3799/dqkx.2022.410

Citation:

Yu Tao, Wang Zongqi, Wang Dongsheng, Liu Xuanyu, Ma Shouxian, Nie Xiao, Ma Changqian, 2023. Provenance and Paleogeographic Significance of Upper Ordovician in NW Zhejiang: Evidence from Sedimentology, Clastic Composition and Chronology. Earth Science, 48(10): 3649-3670. doi: 10.3799/dqkx.2022.410

Citation:

Yu Tao, Wang Zongqi, Wang Dongsheng, Liu Xuanyu, Ma Shouxian, Nie Xiao, Ma Changqian, 2023. Provenance and Paleogeographic Significance of Upper Ordovician in NW Zhejiang: Evidence from Sedimentology, Clastic Composition and Chronology. Earth Science, 48(10): 3649-3670. doi: 10.3799/dqkx.2022.410

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Provenance and Paleogeographic Significance of Upper Ordovician in NW Zhejiang: Evidence from Sedimentology, Clastic Composition and Chronology

doi: 10.3799/dqkx.2022.410

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Development Research Center of China Geological Survey, Beijing 100037, China
3.
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
4.
National Engineering Laboratory for Exploration and Development of Low Permeability Oil and Gas Field, Exploration and Development Research Institute of PetroChina Changqing Oilfield Company, Xi'an 710018, China
5.
School of Earth Science, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-10-29
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

There are many controversies about the Early Paleozoic tectono-sedimentary evolution of the South China plate. The NW Zhejiang is located in the Yangtze block adjacent to the Jiangshan-Shaoxing fault zone, where sedimentary facies transformation of carbonate to clastic rocks occurred in SE Yangtze block during the Late Ordovician. The temporal and spatial distribution of sedimentary facies and provenance analysis can provide evidence for the reconstruction of paleogeography of the SE Yangtze block. Based on detailed analyses of sedimentary facies, sandstone clastic composition, heavy mineral assemblage, geochemistry and detrital zircon U-Pb chronology, in this paper it comprehensively analyzes the provenance of the Upper Ordovician in NW Zhejiang, providing evidence for the reconstruction of paleogeography and tectonic evolution of SE Yangtze block. The Late Ordovician strata in NW Zhejiang are mainly composed of conglomerate, nodular limestone, sandstone, siltstone and mudstone. Sedimentary sequence and facies symbol indicate that the study area was deposited in a deep-sea sloped-shallow sea environment, and the sedimentary basement was inclined to NW. The clastic rocks were mainly composed of lithic sandstones and feldspar lithic sandstones with low compositional and structural maturity and were mainly composed of quartz (29%), feldspar (18%) and lithic (53%). Sandstone clasts and gravel are mainly composed of andesite, rhyolite, tuff, granite, slate, phyllite, quartzite, siltstone and chert, indicating a mixed source. The presence of pyroxene, chromite, magnetite and garnet grains indicates that the source rocks contain mafic and metamorphic rocks. The geochemical analysis shows that the sandstones and siltstones were deposited in active continental margin environment, and the provenance is intermediate acid island arc. The detrital zircon U-Pb ages show a mixed source of ca. 812 Ma and ca. 460 Ma, and the Early Paleozoic provenance can be matched with the Chencai Group. The paleocurrent indicates an SE origin, the provenance comes primarily from the island arc, and the SE Yangtze block was deposited in an active continental margin.
- sedimentary facies,
- provenance,
- Upper Ordovician,
- active continental margin,
- NW Zhejiang,
- geochemistry,
- petrology

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致谢: 感谢中国地质科学院地质研究所闫臻研究员在野外及室内工作中给予的帮助.同时感谢审稿专家与本刊编辑对本文提出的宝贵建议和指导.

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