大陆铀成矿区大地构造类型及其简要评价
The Geotectonic Types of the Continent Uranium Region and Their Brief Evaluation

DOI: 10.12677/AG.2020.105034, PP. 374-384

Keywords: 大陆，铀成矿区，大地构造类型，活化区，简要评价
Continent, Uranium Region, Geotectonic Type, Activated Region, Brief Evaluate

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Abstract:

铀资源量大于2万t的主要大陆铀成矿区约72处，形成于不同成矿时代，产于不同大地构造层内。本文以铀成矿区为载体，依据大地构造控矿观点，提出大陆铀成矿区大地构造类型划分，分出5大类15亚类27小类。大类划分是按成矿区大地构造层的属性不同，亚类划分是按铀成矿区的铀成矿时代差别，小类划分是按成矿区的局部构造及含矿主岩类别的区分，并对铀成矿区主要大地构造类型作简要评价。这种划分在进行铀成矿区评价时较为方便适用，有一定的参考意义。
About 72 continental uranium regions with a uranium resource of more than 20,000 t are formed in different mineralogentic epoches and occur in different tectonic layers. Based on the geotectonic ore-controlling point of view, this paper proposes the classification of geotectonic types in continental uranium mining area, which is divided into 5 categories, 15 sub-categories and 27 subclasses. The classification is based on the different attributes of the geotectonic strata in the mining area, the sub-categories are based on the time of uranium mineralization in the uranium mining area, the subclasses are divided according to the local tectonics and the main ore-bearing rock types in the mining area, and the main geotectonic types in the uranium mining area are briefly evaluated. This division is convenient and applicable in the evaluation of uranium mining area, and has certain reference significance.

References

[1]	Ю.М.Шувалов и др. (1980) Металлогения урана котинетальных блоков Земной коры. ИздаТельство “Недра”, 20-195.
[2]	Ю.М.Шувалов и др. (1984) Промышленые типы урановых месиорождений и методика их пойсков Москова. 13-25.
[3]	Bеличкин, B.И. (1983) Oсобености металлогении ураноносных областей. Энергоатом Издат, Москва, 125-195.
[4]	Бойцов, В.Е. andВерчеба, А.А. (2008) Геолого-промышленые типы месиорождений урана. Универстет книжный дом, Москва, 29-279.
[5]	A.H.G.Mitchell, M.S.Garson. 矿床与全球构造[M]. 北京: 地质出版社, 1986: 21-198.
[6]	姚振凯, 黄宏业, 刘翔. 新世纪陆壳新增铀成矿区及其简要特征[J]. 中南铀矿地质, 2019, 23(2): 60-64.
[7]	Liu, X.D. (2018) New Uranium Deposits and Innovation Technologies for Uranium Exploration. East China University of Technology, Fuzhou, 4-64.
[8]	陈国达, 杨心宜. 活化构造成矿学[M]. 长沙: 湖南教育出版社, 2003: 171-246+602-643.
[9]	姚振凯, 刘翔, 郑大瑜. 亚欧东西向活化构造铀成矿带划分依据及铀成矿域分布[J]. 铀矿地质, 2014, 30(4): 193-199.
[10]	Dahlkamp, F.J. (1991) Uranium Ore Deposits. Springer, Berlin, Heidelberg, New York, 324-330.
[11]	姚振凯. 我国铀矿床的大地构造类型及其主要特征[J]. 大地构造与成矿学, 1983, 7(2): 117-125.
[12]	Л.В. Григоръева. (1986) Докембрийская тестоно-магматическая активизация. Недра, Ленинград, 33-112.
[13]	赵凤民. 欧亚大陆铀区域成矿模式[M]. 北京: 核工业北京地质研究院, 2016: 27-30+80-94+138-149.
[14]	姚振凯, 范立亭, 黄宏业. 俄罗斯铀矿地质工作新进展[J]. 世界核地质科学, 2017, 34(4): 194-199.
[15]	И.Г.Печенкин. (2003) Металлогения Туранской плиты. Москва, ВИМС, 14-45. https://doi.org/10.1093/combul/45.6.14
[16]	Yao, Z.K., Liu, Y.H., Zhu, R.B., Yang, S.H. and Li, D.P. (1989) Uranium Metallogenesis in Southeast China. Metallogenesis of Uranium Deposis. IAEA, Vienna, 345-356.
[17]	黄净白, 黄世杰, 张金带, 等. 中国铀成矿带概论[M]. 北京: 中国核工业地质局, 2005: 75-83+215-244.
[18]	А.Д.Щеглов. (1971) Металлогения срединных массивов. Изд. нера, Москва, 20-48+72-78.
[19]	姚振凯, 范立亭, 黄宏业, 等. 亚欧大陆东西向活化构造带中间地块铀成矿特征[J]. 世界核地质科学, 2019, 36(1): 1-9.
[20]	姚振凯. 中国地洼区层控铀矿床地质和分布规律[J]. 矿床地质, 1982, 1(1): 83-88.

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