金属矿床的成矿流体成分和流体包裹体
Composition of ore forming fluids in metal deposits and fluid inclusion
查看参考文献41篇
|
文摘
|
自然界中的成矿流体按其主要成分,可分为: (1)岩浆,即形成岩浆矿床的岩浆; (2)以H_2O为主的流体(含NaCl) ; (3)以CO_2为主的流体。地壳中的流体类型很多,只有含一定金属元素含量的,并且达到一定浓度时才称为金属矿床的成矿流体。基于对矿床中流体包裹体和天然成矿流体中金属种类和含量的测定,这些金属矿床的成矿流体按金属元素含量可以分为五组,成矿流体可以来自岩浆、岩浆热液、大气降水、盆地卤水和变质流体等地质环境。 |
|
其他语种文摘
|
Ore forming hydrothermal fluids,consisting largely of silicate melt,H_2O,CO_2 and NaCl,formed most of Earth’s mineral deposits. The ore forming fluids exist as magma,magmatic fluids,meteoric water,seawater,basinal brine,and metamorphic fluids. The metal concentration of the ore forming fluids could be classified into 5 groups according to their geochemical features and metal amounts in the fluids. These were approved by the fluid inclusion and nature ore forming fluids analysis. |
|
来源
|
岩石学报
,2015,31(4):1108-1116 【核心库】
|
|
关键词
|
成矿流体
;
金属元素含量
;
流体包裹体
|
|
地址
|
1.
Science de la terre,University of Quebec, Chicoutimi, G7H 2B1
2.
中国科学院广州地球化学研究所, 广州, 510640
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
1000-0569 |
|
学科
|
地质学 |
|
基金
|
国土资源部公益性行业科研专项经费
;
中国科学院贵阳地球化学研究所矿床地球化学中国科学院重点实验室基金
|
|
文献收藏号
|
CSCD:5454814
|
参考文献 共
41
共3页
|
|
1.
Appold M S. Limits on the metal content of fluid inclusions in gangue minerals from the Viburnum trend, SE Missouri determined by LA-ICP-MS.
GSA Annual Meeting, Denver (Oct. 27-30, 2002), Abstract Volume,2002
|
CSCD被引
1
次
|
|
|
|
|
2.
Appold M S. Composition of ore fluid inclusions from the Viburnum trend.
Economic Geology,2011,106(1):55-78
|
CSCD被引
9
次
|
|
|
|
|
3.
Audetat A. Causes for large-scale metal zonation around mineralized plutons:Fluid inclusion La-ICPMS evidence from the Mile Granite, Australia.
Econ. Geol,2000,95:1563-1581
|
CSCD被引
27
次
|
|
|
|
|
4.
Baker T. Composition and evolution of ore fluids in a magmatic-hydrothermal skarn deposit.
Geology,2003,32(2):117-120
|
CSCD被引
66
次
|
|
|
|
|
5.
Banks D A. Emerald mineralisation in Columbia:Fluid chemistry and the role of brine mixing.
Mineralium Deposita,2000,35:699-713
|
CSCD被引
2
次
|
|
|
|
|
6.
Barnes H L.
Geochemistry of Hydrothermal Ore Deposits. (3~(rd) Edition),1997
|
CSCD被引
1
次
|
|
|
|
|
7.
Bottrell S H. A modified crush-leach method for the analysis of fluid inclusion electrolytes.
Bulletin de Mineralogie,1988,111:279-290
|
CSCD被引
1
次
|
|
|
|
|
8.
Campbell A R. Geochemistry of Th-U-REE mineralizing magmatic fluids, Capitan Mountains, New Mexico.
Econ. Geol,1995,90:1271-1287
|
CSCD被引
4
次
|
|
|
|
|
9.
Carpenter A B. Preliminary report on the origin and chemical evolution of lead and zinc rich oil-field brines in Central Mississippi.
Econ. Geol,1974,69:1191-1206
|
CSCD被引
8
次
|
|
|
|
|
10.
Connolly C A. Origin and evolution of formation waters, Alberta basin, western Canada sedimentary basin I.
Chemistry, Applied Geochemistry,1990,5:373-395
|
CSCD被引
1
次
|
|
|
|
|
11.
Frape S K. Geochemical trends from groundwaters from the Canadian Shield.
Geological Association of Canada Special Paper,1987,33:19-38
|
CSCD被引
2
次
|
|
|
|
|
12.
Graton L C. Nature of the ore-forming fluid.
Economic Geology,1940,35(Suppl. 2):197-358
|
CSCD被引
1
次
|
|
|
|
|
13.
Hedenquist J W. The role of magmas in the formation of hydrothermal ore deposits.
Nature,1994,370(6490):519-527
|
CSCD被引
331
次
|
|
|
|
|
14.
Heinrich C A. Segregation of ore metals between magmatic brine and vapor:A fluid inclusion study using PIXE microanalysis.
Economic Geology,1992,87(6):1566-1583
|
CSCD被引
56
次
|
|
|
|
|
15.
Kamenetsky V S. Extreme heterogeneity of granite derived hydrothermal fluids:An example from inclusions in a single crystal of miarolitic quartz.
Geology,2002,30:459-462
|
CSCD被引
10
次
|
|
|
|
|
16.
Kasai K. Supersaline brine obtained from Quaternary Kakkonda granite by the Nedos deep geothermal well WD-1A in the Kakkonda geothermal field, Japan.
Geothermal Resources Council Transactions,1996,20:623-629
|
CSCD被引
1
次
|
|
|
|
|
17.
Kesler S E. Ore-forming fluids.
Elements,2005,1(1):13-18
|
CSCD被引
26
次
|
|
|
|
|
18.
Land L S. The geochemistry of saline formation waters, Miocene, offshore Louisiana, Gulf Cost.
Association of Geological Societies, Transactions,1988,38:503-511
|
CSCD被引
1
次
|
|
|
|
|
19.
Lerchbaumer L. The metal content of molybdenummineralizing fluids.
EGU General Assembly 2012, held 22-27 Apirl, 2012 in Vienna,2012:P11889
|
CSCD被引
1
次
|
|
|
|
|
20.
McCaig A M. Fluid mixing and recycling during Pyrenean thrusting:Evidence from fluid inclusion halogen ratios.
Geochimica et Cosmochimica Acta,2000,64:3395-3412
|
CSCD被引
1
次
|
|
|
|
|
了解气象卫星更多信息，请访问