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Magnetite-Fluorite Rock: A New Rock Type of Hot Water Sedimentation

XU Shaokang XIA Xuehui YUAN Congjian WANG Bingquan YAN Fei YAN Shengxian ZHENG Xingquan

地质学报(英文版)2008,Vol.82Issue(4):906-910,5.
地质学报(英文版)2008,Vol.82Issue(4):906-910,5.

Magnetite-Fluorite Rock: A New Rock Type of Hot Water Sedimentation

Magnetite-Fluorite Rock: A New Rock Type of Hot Water Sedimentation

XU Shaokang 1XIA Xuehui 1YUAN Congjian 2WANG Bingquan 2YAN Fei 1YAN Shengxian 3ZHENG Xingquan3

作者信息

  • 1. Geological Institute of China Chemical Geology and Mine Bureau, Zhuozhou 072754
  • 2. China Chemical Geology and Mine Bureau, Beijing 100101
  • 3. Zhejiang Geological Exploration Institute of China Chemical Geology and Mine Bureau, Zhejiang 310002
  • 折叠

摘要

Abstract

The new type hot water sedimentary rock - magnetite-fluorite rock occurs as quasi-layers inflat parts of contact zones between rock body and strata in Bamiaushan of Changshan County,Zhejiang Province, China. The main mineral assemblage is fluorite+magnetite+cassiterite. The rockshows typical laminated structure and obvious mosaic texture. Its formation temperature is between123℃-160℃, averaging at 142℃. The major chemical composition of the rock includes CaF2, SiO2,Al2O3, FeO, and Fe2O3; the high-content microelement association includes W, Sn, Be, Rb, Sr, S, andCl; and the total content of REE is low (∑REE between 35.34x10-6-38.35x10-6), showing LREEenrichment type of distribution pattern. Diagenesis: driven by the tectonic stress, the formation waterheated in the deep strata had moved along the fissures or fractures in strata and had extractedcomponents from the strata on the way, and finally stagnated in the flat parts of contact zones betweenrock body and strata. With drop in temperature, magnetite and fluorite were separated from the hotwater and precipitated alternately, forming this hot water sedimentary rock with new typemineralogical composition, typical laminated structure, obvious mosaic texture and sub-horizontaloccurrence. The characteristics of the new type mineralogical composition, sedimentary tectonicenvironment and chemical composition are different from that of the well-known traditionalhydrothermai sedimentary rocks.

关键词

magnetite-fluorite rock, hot water sedimentary rock, hydrothermai sedimentary rock,laminated structure, sedimentary tectonic environment, petrochemistry

Key words

magnetite-fluorite rock, hot water sedimentary rock, hydrothermai sedimentary rock,laminated structure, sedimentary tectonic environment, petrochemistry

分类

天文与地球科学

引用本文复制引用

XU Shaokang,XIA Xuehui,YUAN Congjian,WANG Bingquan,YAN Fei,YAN Shengxian,ZHENG Xingquan..Magnetite-Fluorite Rock: A New Rock Type of Hot Water Sedimentation[J].地质学报(英文版),2008,82(4):906-910,5.

基金项目

This work is supported by the Project of China Chemical Geology and Mine Bureau. ()

地质学报(英文版)

OACSCD

1000-9515

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