TERRESTRIAL HEAT-FLOW IN EASTERN ARIZONA - 1ST REPORT

被引：14

作者：

REITER, M

SHEARER, C

机构：

[1] NEW MEXICO INST MIN & TECHNOL, NEW MEXICO BUR MINES & MINERAL RESOURCES, SOCORRO, NM 87801 USA

[2] NEW MEXICO INST MIN & TECHNOL, DEPT GEOSCI, SOCORRO, NM 87801 USA

来源：

JOURNAL OF GEOPHYSICAL RESEARCH | 1979年 / 84卷 / NB11期

关键词：

D O I：

10.1029/JB084iB11p06115

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Fifteen heat-flow measurements are presented for eastern Arizona and neighboring areas. In the Gila Mountains of southeastern Arizona a heat flow of 1.9 HFU (the approximate average for the Basin and Range Province) is estimated for the best measurements. In the eastern part of the Safford Valley, just south of Gila Mountains, subsurface temperature gradients were measured at one site to 1050m. Heat-flow data from this site, considered with the reported hydrogeology and hot spring activity of the valley fill deposits, suggest complex hydrothermal phenomena in the valley. Several hundred km to the north, high heat flows (more than 2.5 HFU) are observed within the Mogollon Slope of the Colorado Plateau. - Authors

引用

页码：6115 / 6120

页数：6

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