干旱区生态环境知识资源中心(Arid): Chemical evolution of a high-level magma system: the Black Mountain volcanic center, southern Nevada

Arid

DOI	10.2172/6990064
报告编号	UCRL-53444
来源ID	OSTI_ID: 6990064
	Chemical evolution of a high-level magma system: the Black Mountain volcanic center, southern Nevada
	Vogel, T.A.; Noble, D.C.; Younker, L.W.
英文摘要	A comprehensive study of stratigraphically controlled samples of both lavas and ash-flow tuffs from the Black Mountain volcanic center enables us to evaluate magmatic processes. The results of this study are used to: (1) determine how this high-level magma system developed; (2) compare this system with other similar systems; and (3) correlate ash-flow sheets using their chemical characteristics.
出版年	1983
报告类型	Technical Report
语种	英语
国家	美国
来源学科分类	15 GEOTHERMAL ENERGY ; MAGMA SYSTEMS ; GEOLOGIC HISTORY ; NEVADA ; ASHES ; LAVA ; STRATIGRAPHY ; TUFF ; VOLCANIC REGIONS ; FEDERAL REGION IX ; GEOLOGY ; GEOTHERMAL SYSTEMS ; NORTH AMERICA ; RESIDUES ; USA Geothermal Legacy 150201* -- Geology & Hydrology of Geothermal Systems-- USA-- (-1989)
URL	http://www.osti.gov/scitech/servlets/purl/6990064
资源类型	科技报告
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/263520
推荐引用方式 GB/T 7714	Vogel, T.A.,Noble, D.C.,Younker, L.W.. Chemical evolution of a high-level magma system: the Black Mountain volcanic center, southern Nevada,1983.