HEAT-FLOW FIELD IN MAINLAND UK

被引：26

作者：

RICHARDSON, SW

OXBURGH, ER

机构：

[1] Department of Geology and Mineralogy, University of Oxford, Oxford, Parks Road

[2] Department of Mineralogy and Petrology, University of Cambridge, Cambridge, Downing Place

来源：

NATURE | 1979年 / 282卷 / 5739期

关键词：

D O I：

10.1038/282565a0

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Belts of relatively high flux correspond to zones of crust enriched in radioactive heat production to ∼15 km depth. The enrichments were introduced into the crust by granitic magmas. © 1979 Nature Publishing Group.

引用

页码：565 / 567

页数：3

共 37 条

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[22]

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[28]

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[29] HEAT GENERATION OF PLUTONIC ROCKS AND CONTINENTAL HEAT FLOW PROVINCES [J].

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BLACKWEL.DD ;

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[30] IMPLICATIONS OF TERRESTRIAL HEAT FLOW OBSERVATIONS ON CURRENT TECTONIC AND GEOCHEMICAL MODELS OF CRUST AND UPPER MANTLE OF EARTH [J].

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GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1970, 20 (05) :509-+

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