Premium
A Study of Wajiertag Magmatic Deposit Based on Magnetic Anomalies
Author(s) -
HUANG Xuzhao,
FAN Zhengguo,
YANG Xue,
ZHOU Daoqing,
LIU Qiankun,
LI Shuqin
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 - 10.1111/1755-6724.12371_9
Subject(s) - beijing , china , remote sensing , geophysical survey , chinese academy of sciences , geological survey , geology , center (category theory) , geography , seismology , geophysics , archaeology , chemistry , crystallography
The mineralization associated with the continental flood basalt has long been enjoying close attention,Which is considered to be most promising magmatic deposit type in China. The Panzhihua magmatic V-Ti-Fe deposit is one of the typical examples(Zhang, 2014; Tang, 2004). Because the Permian massive mafic eruptive events happened in the margin of Tarim ancient land, the flood basalts and mafic and ultramafic rocks were distributed. Wajiertag magmatic V-Ti-Fe deposit is located 45 km outside the Bachu to the southeast. Despite of the similarity with Panzhihua deposit in terms of ore-forming geological condition, the features of magnetic anomalies are considerably different. Combined with geophysical and geological studies, the results indicate that Wajiertag iron deposit is formed through the later-stage Fe-rich mafic magma intrusion and evolution after intrusion of gabbro. In this paper, we aim to provide useful information for magmatic V-Ti-Fe deposit.