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Characteristics of mantle branch structure in western Shandong and its roles in minerogenesis and ore-controlling

SUN Aiqun HU Huabin NIU Shuyin MAO Jingwen WANG Debao LI Yingping WANG Laiming

中国地球化学学报(英文版)2006,Vol.25Issue(4):340-353,14.
中国地球化学学报(英文版)2006,Vol.25Issue(4):340-353,14.

Characteristics of mantle branch structure in western Shandong and its roles in minerogenesis and ore-controlling

Characteristics of mantle branch structure in western Shandong and its roles in minerogenesis and ore-controlling

SUN Aiqun 1HU Huabin 1NIU Shuyin 1MAO Jingwen 2WANG Debao 3LI Yingping 1WANG Laiming4

作者信息

  • 1. Institution of Geological Survey, Shijiazhuang University of Economics, Shijiazhuang 050031, China
  • 2. Chinese University of Geosciences, Beijing 100083, China
  • 3. Institute of Mineral Resources, Chinese Academy of Geosciences, Beijing 100037, China
  • 4. Institution of Provincial Geological Survey, Shandong, Ji'nan 250013, China
  • 折叠

摘要

Abstract

This work deals with the characteristics of mantle branch structure in western Shandong Province, China, with respect to the distribution characteristics and ages of the regional strata, the development of ring-like and radial faults, the development of gently inclined detachment-slip structures in the axial part, mantle-source magmatic activities, regional petrology, petrochemistry and isotope geology. The study indicated that the N-W sharply plunged ductile shear zone in the region of western Shandong cuts through the mantle rocks detached from the deep-seated North China mantle sub-plume, hence leading to unloading in response to depressurization and thereafter the formation of anatexis magma. The intense and complete magmatic evolution series not only manifests a variation trend of alkalinity of magma from high to low and its intrusive depth from deep to shallow, but also reflects that the wall-rock alteration shows a general evolution trend from strong to weak. The evolution of mantle structure played an important role in controlling endo-mineralogenesis, accompanied with the rise of the country rocks. As a result, typical mantle branch structures were formed as observed in western Shandong. At the top of the mantle branch structure was developed an obvious detachment-tilt fault block, and some endogenic ores, at the same time, were uplifted onto the shallow levels.

关键词

mantle branch structure/mantle plume/tectonic evolution/tectonic ore-controlling/minerogenesis/region of western Shandong Province

Key words

mantle branch structure/mantle plume/tectonic evolution/tectonic ore-controlling/minerogenesis/region of western Shandong Province

分类

天文与地球科学

引用本文复制引用

SUN Aiqun,HU Huabin,NIU Shuyin,MAO Jingwen,WANG Debao,LI Yingping,WANG Laiming..Characteristics of mantle branch structure in western Shandong and its roles in minerogenesis and ore-controlling[J].中国地球化学学报(英文版),2006,25(4):340-353,14.

基金项目

This research project was financially supported jointly by the National Natural Science Foundation of China (Grant No. 40272088), the Large-scale Geological Survey in China (No. 2000110100038) and the Central Mining Funds (2003-20). (Grant No. 40272088)

中国地球化学学报(英文版)

2096-0956

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