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The abundance of mercury in rocks, minerals and native sulphur by a microwave-excited argon plasma

Identifieur interne : 000185 ( Istex/Corpus ); précédent : 000184; suivant : 000186

The abundance of mercury in rocks, minerals and native sulphur by a microwave-excited argon plasma

Auteurs : R. K. Srivastava

Source :

RBID : ISTEX:5877AD53F0AF1052948BB95649C5EBB6C98D321D

English descriptors

Abstract

Abstract: Igneous rocks, silicate minerals and native sulphur have been analysed for their mercury content by a microwave-excited argon plasma. Basic and ultrabasic igneous rocks have abundances between 3 and 31 ppb Hg. The granitic rocks show much larger variations. The content in the silicate minerals is highly variable, ranging from less than 1 ppb Hg in an igneous biotite to 55 ppb Hg in a pegmatitic biotite. The analysed clay minerals give 110 and 200 ppb Hg. Volcanic elemental S contain from 11 to 9300 ppb Hg, the values on the lower side being from oceanic volcanoes and on the higher side for continental or marginal volcanoes.

Url:
DOI: 10.1016/0009-2541(79)90043-3

Links to Exploration step

ISTEX:5877AD53F0AF1052948BB95649C5EBB6C98D321D

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