|Table of Contents|

New Insight into the Mesoproterozoic Stratigraphic Tectonic Framework in the Southwestern Margin of North China Craton(PDF)

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

Issue:
2025年第02期
Page:
158-175
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
New Insight into the Mesoproterozoic Stratigraphic Tectonic Framework in the Southwestern Margin of North China Craton
Author(s):
ZHOU Yi-jun1*;  LI Zhen-hong2; 3;  BAI Hai-feng4;  YU Xiao-lei1;  DONG Xiao-peng2; 3;  KOU Lin-lin2; 3
(1. Geophysical Research Institute, BGP Inc., CNPC, Zhuozhou 072750, Hebei, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 3. Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China; 4. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, Shaanxi, China)
Keywords:
Mesoproterozoic;  Changcheng System;  Xiong'er Group;  basaltic andesite;  geochemistry;  rift system;  North China Craton
PACS:
P534.3; P548
DOI:
10.19814/j.jese.2024.10004
Abstract:
The three rift systems of Xiong'er rift in the southern margin, Yanliao rift in the northeastern margin and Zha'ertai-Baiyun'ebo rift in the northern margin of North China Craton have been recognized by the geoscience community. However, whether there is a Guyuan rift in the southwestern margin has been questioned due to the lack of direct evidence of large-scale volcanic eruption. Based on the latest drilling core cuttings data of well Pantan1, combined with regional seismic profiles, zircon U-Pb dating and element geochemical analysis, the eruption time and tectonic attributes of the Mesoproterozoic Changcheng System volcanic rocks were determined; the Mesoproterozoic sedimentary-volcanic rock sequence in the southwestern margin of North China Craton and its correlation with Changcheng System in Zhongtiaoshan area of Xiong'er rift were systematically established, and the geological structure of the Mesoproterozoic in the southwestern margin of North China Craton was revealed. The results show that a set of thick basaltic andesite is drilled in well Pantan1 in the Mesoproterozoic Changcheng System; the basaltic andesite has inter-cryptic structure and glass-based porphyritic structure, mainly glassy and basic plagioclase, containing abundant magnetite; the main eruption time of volcanic rock is(1 768.51±0.39)Ma and(1 778.7±8.0)Ma, respectively, which is equivalent to the volcanic rock sequence of Majiahe Formation in Xiong'er rift in Zhongtiaoshan area, the southern margin of North China Craton; the element geochemical characteristics of the basaltic andesite show LREE enrichment, HREE loss, Eu negative anomaly, trace elements are relatively enriched in large ion lithophile elements Rb and Th, Zr and Hf obvious positive anomalies, Sr, P, Ba, Ti, Nb obvious negative anomalies, with a regional extensional tectonic background; on the seismic profile, the difference of wave velocity between the basaltic andesite and the overlying sandstone is obvious, which can form a strong trough reflection interface and is conducive to the accurate calibration and tracking of the basaltic andesite; the seismic and drilling are mutually constrained, and the main range of the Mesoproterozoic volcanic facies is effectively delineated; it is roughly located between Guyuan and Yinchuan on the western margin of North China Craton.

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Last Update: 2025-03-20