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A Preliminary Study of Manganese Mineralization Model in Changyang Region, Hubei Province
Author(s) -
GUO Wei,
CHEN Mengjie,
YANG Hongwei,
LIU Hai,
ZHOU Minyue
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12367_4
Subject(s) - mineralization (soil science) , geography , library science , archaeology , geology , soil science , computer science , soil water
The study area is located in the northern edge of the Yangtze platform and the core parts of the Changyang anticline (Zhang et al., 2013). It has developed the ancient North-south trending fault which is influenced by Yangtze plate extension. This fault has formed a nearly Northsouth trending faulted basin and block uplift in this area. Besides, due to the development of the Tianyangping ancient fracture, and its influence, the study area has also developed the north-west ancient fracture, whose main performance is lifting. So, affected by the above two kinds of faulting together, the checkerboard faulted basin formed, such as Gucheng basin, Paomaping basin, Huangjiaping basin and so on. These faulted basin accepted manganese sedimentation, developing into manganese basin.