SURFACE HYDROTHERMAL MINERALS AND THEIR DISTRIBUTION IN THE TENGCHONG   GEOTHERMAL AREA, CHINA

doi:10.1016/0375-6505(87)90065-4

CORC > 北京大学 > 地球与空间科学学院

	SURFACE HYDROTHERMAL MINERALS AND THEIR DISTRIBUTION IN THE TENGCHONG GEOTHERMAL AREA, CHINA
	ZHU, MX ; TONG, W
刊名	geothermics
	1987
DOI	10.1016/0375-6505(87)90065-4
英文摘要	In the active hydrothermal areas of Tengchong there is widespread evidence that hydrothermal minerals are deposited directly from the geothermal fluid or from water-rock interactions. X-ray powder diffraction, electron microprobe analyses and classical optical methods were used to identify these hydrothermal minerals. Sulfates (gypsum, alunite, alunogen, halotrichite, etc. ), carbonates (calcite, trona, thermonatrite, etc. ), clay minerals (kaolinite, illite-smectic mixed layer mineral, etc. ) and silica minerals (opal, chalcedony, etc. ) are the dominant phases. Native sulfur, pyrite, marcasite and aragonite are next in order of abundance. Some chabazite, analcime, pitchblende, coffinite, hematite, thenardite, rozenite, coquimbite, manganocalcite and rhodochrosite is also present.; Energy & Fuels; Geosciences, Multidisciplinary; SCI(E); EI; 13; ARTICLE; 2; 181-195; 16
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/311014]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	ZHU, MX,TONG, W. SURFACE HYDROTHERMAL MINERALS AND THEIR DISTRIBUTION IN THE TENGCHONG GEOTHERMAL AREA, CHINA[J]. geothermics,1987.
APA	ZHU, MX,&TONG, W.(1987).SURFACE HYDROTHERMAL MINERALS AND THEIR DISTRIBUTION IN THE TENGCHONG GEOTHERMAL AREA, CHINA.geothermics.
MLA	ZHU, MX,et al."SURFACE HYDROTHERMAL MINERALS AND THEIR DISTRIBUTION IN THE TENGCHONG GEOTHERMAL AREA, CHINA".geothermics (1987).