|Table of Contents|

Provenance Characteristics of Upper Triassic-Middle Jurassic in the Eastern Kuqa Depression of Tarim Basin, China and Their Geological Significance(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2020年第02期
Page:
172-187
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Provenance Characteristics of Upper Triassic-Middle Jurassic in the Eastern Kuqa Depression of Tarim Basin, China and Their Geological Significance
Author(s):
XU Xing-bin1;  WANG Chang-yong1*;  LIU Man-cang2;  LIN Shi-guo2;  LI De-jiang2;  GAO Zhi-yong3
(1. Institute of Sedimentany Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. Langfang Branch of Research Institute of Petroleum Exploration and Development, PetroChina, Langfang 065007, Hebei, China; 3. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China)
Keywords:
provenance analysis;  tectonic evolution;  heavy mineral;  cathodoluminescence;  Triassic;  Jurassic;  South Tianshan;  Tarim Basin
PACS:
P588.2
DOI:
10.19814/j.jese.2019.11041
Abstract:
Based on the analysis results of thin sections, cathodoluminescence of quartz and heavy mineral assemblages, combined with sedimentary structures and seismic reflection characteristics, the provenance direction, parent rocks and evolution characteristics of Upper Triassic-Middle Jurassic in the eastern Kuqa depression of Tarim Basin were studied. The results show that the provenance of Upper Triassic-Middle Jurassic in the eastern Kuqa depression of Tarim Basin is mainly from South Tianshan orogenic belt in the north, and the parent rocks are mainly magmatic and metamorphic with a few sedimentary. Among them, there is a higher content of terrigenous clastic lithic and quartz without luminescence in the sandstone of Taliqike Formation, and the heavy mineral assemblages are characterized by higher contents of zircon, leucosphenite and magnetite, and lower contents of garnet, indicating that the parent rocks may be early deposition of Upper Ordovician-Upper Triassic; the contents of magmatic rock lithic in the sandstone of Ahe Formation and Yangxia Formation increase, the heavy minerals are characterized by higher contents of garnet, and quartz mainly gives off blue-purple and tan light under the condition of cathodoluminescence, indicating that the parent rocks of Ahe Formation and Yangxia Formation mainly come from Permian and its underlied sediments; the contents of metamorphic rock lithic and quartz with tan luminescent in the sandstone of Kezilenu'er Formation and Qiakemake Formation increase obviously, and the content of garnet is extremely high, indicating that the influence of metamorphic parent rock is enhanced. The evolution of parent rocks in the provenance area of Late Triassic-Middle Jurassic has obvious regularity. The parent rocks are mainly sedimentary in Late Triassic, and the contents of magmatic parent rocks increase in Early Jurassic, and finally, it is characterized by metamorphic parent rocks in Middle Jurassic. In Late Triassic, the South Tianshan orogenic belt is greatly uplifted in the eastern Kuqa depression, as a result, a large number of metamorphic parent rocks are involved in the orogenic belt and denuded; in Early-Middle Jurassic, the tectonic activity in the middle section of South Tianshan orogenic belt is characterized by east and west sections, the sandstone in the eastern region firstly has high content of garnet in Early Jurassic, while the sandstone in the western region does not appear garnet abundance until Middle Jurassic. It shows that Hula and E'erbin mountains in the middle section of South Tianshan orogenic belt are uplifted and denuded strongly in Early Jurassic, but Halke mountain is uplifted consumingly in Middle Jurassic.

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Last Update: 2020-03-24