Published April 2018 | Version v1
Book

Uranium metallogenic conditions evaluation of Xinchengzi secondary volcanic basin in Daban basin of Inner Mongolia

  • 1. Geological Party No. 243, CNNC, Chifeng, Inner Mongolia (China)

Description

Xinchengzi secondary volcanic basin is in Daban basin which is located to the south of the Zhalantun volcanic-rock related uranium mineralization prospect. Meanwhile, it is part of Huanggangliang-Ulanhot polymetallic metallogenic belt. The tectonic location, basement and uranium concentration, structural features, magmatic activity, wall rock alteration and uranium mineralization characteristics of the cover were analyzed based on the tectonic position, strata, intrusive rocks, structure and basic geological characteristics of uranium mineralization features. With these analyses, the author thinks that the secondary volcanic basin has good metallogenic potential. (authors)

Part of:
Progress report on nuclear science and technology in China (Vol.5). Proceedings of academic annual meeting of China Nuclear Society in 2017, No.1--Uranium Geology sub-volume

Additional details

Publishing Information

Publisher
China Atomic Energy Press
Imprint Place
Beijing (China)
ISBN
978-7-5022-8776-4
Imprint Title
Progress report on nuclear science and technology in China (Vol.5). Proceedings of academic annual meeting of China Nuclear Society in 2017, No.1--Uranium Geology sub-volume
Imprint Pagination
474 p.
Journal Page Range
p. 39-45

Conference

Title
2017 academic annual meeting of China Nuclear Society
Dates
16-18 Oct 2017
Place
Weihai (China)

INIS

Country of Publication
China
Country of Input or Organization
China
INIS RN
53101908
Subject category
S11: NUCLEAR FUEL CYCLE AND FUEL MATERIALS; S58: GEOSCIENCES;
Resource subtype / Literary indicator
Conference
Descriptors DEI
CHINA; CONCENTRATION RATIO; EVALUATION; MINERALIZATION; PLUTONIC ROCKS; TECTONICS; URANIUM; VOLCANIC ROCKS
Descriptors DEC
ACTINIDES; ASIA; DIMENSIONLESS NUMBERS; ELEMENTS; IGNEOUS ROCKS; METALS; ROCKS

Optional Information

Notes
9 figs., 7 refs.