Source(s) and Distribution of Metals in Porphyry Copper Deposits
Source(s) and Distribution of Metals in Porphyry Copper Deposits
批准号:
9316051
负责人:
Robert Bodnar
金额:
$10.0万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1994
资助国家:
美国
项目状态:
已结题
起止时间:
1994-03-01 至 1996-08-31
中文摘要
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英文摘要
9316051 Bodnar The porphyry copper deposits are major producers of copper as well as molybdenum, zinc, lead, gold, silver, arsenic, selenium and other metals. It is proposed to investigate sources of the metals in porphyry copper deposits by conducting synchrotron XRF (SXRF) analyses of carefully selected fluid inclusions from 6 ore deposits representing a wide range in vertical and lateral positions within the larger magmatic-hydrothermal system. Preliminary SXRF analyses of samples from the Red Mountain and Morenci, AZ, and the Santa Rita, NM., porphyry systems document the feasibility of conducting nondestructive analyses of individual fluid inclusions from these deposits. Most of the samples to be studied have previously been characterized through detailed petrography, microthermometric and geochemical analysis, and their position within the paragenetic sequence and their relationship to hypogene copper mineralization are well understood. Results from this study will improve our understanding of the genesis of this important ore deposit type by identifying which fluids are carrying metals and where these fluids are distributed vertically and laterally within the magmatic-hydrothermal system.
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Experimental Study of Water Leakage from Melt Inclusions in Quartz During Laboratory Heating
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资助金额:$19.97万
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Development of a Numerical Model for the PVTX Properties of Na-K-Ca-Fe-C1 Solutions in Magmatic/Hydrothermal Ore Deposits
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批准号:0125918
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资助金额:$33.65万
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Melt Inclusions in Zircon (and other accessory minerals)
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批准号:9725248
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资助金额:$13.04万
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财政年份:1998
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Upgrade of Hydrothermal Facilty
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批准号:9614272
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财政年份:1997
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依托单位:
Accomplishment-Based Renewal: Source(s) and Distribution of Metals in Porphyry Copper Deposits
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批准号:9527034
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项目类别:Continuing Grant
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资助金额:$16.03万
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财政年份:1996
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Fluid Inclusions as Recorders of Tectonic History
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