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Geologic Features of Yongqu Iron Ore, Nierong County, North Tibet
Author(s) -
LI Shanglin,
MA Boyong,
LUO Yanjun,
MA Zhongping,
QIAO Gengbiao
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_7
Subject(s) - geological survey , beijing , china , geology , center (category theory) , archaeology , mining engineering , geochemistry , geography , paleontology , chemistry , crystallography
Yongqu iron ore is located in the northern to Dangqu River upstream, Nierong County, 24 km south to Yongqu Town. Integrated brigade, Tibet Bureau of Geology and Mineral Resources, conducted the surface inspection and peripheral census work in 1979. This ore has a certain scale and high grade, so it has great value of development and utilization. Regionally, it belongs to the late Paleozoic-Mesozoic Qiangtang Sanjiang tectonic zone (I), Changdu-Mangkang-Simao continental block (II), the Changdu Lanping Mesozoic bidirectional retroarc foreland basin (III) of Pan Cathaysian region(Pan Guitang et al, 2003); Southern China formation region (I), north Qiang-Changdu stratigraphic region (II) and the northern Qiangtang stratigraphic division (III).