EXPERIMENTAL PETROCHEMISTRY OF SOME HIGHLY SIDEROPHILE ELEMENTS AT HIGH TEMPERATURES, AND SOME IMPLICATIONS FOR CORE FORMATION AND THE MANTLES EARLY HISTORY

dc.contributor.author	O'Neill H.S.C.
dc.contributor.author	Dingwell D.B.
dc.contributor.author	Borisov A.
dc.contributor.author	Spettel B.
dc.contributor.author	Palme H.
dc.date.accessioned	2020-12-04T08:47:57Z
dc.date.available	2020-12-04T08:47:57Z
dc.date.issued	1995
dc.identifier	https://elibrary.ru/item.asp?id=31635534
dc.identifier.citation	Chemical Geology, 1995, , 3, 255-273
dc.identifier.issn	0009-2541
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/20415
dc.description.abstract	The highly siderophile elements (HSE's: Ru, Rh, Pd, Re, Os, Ir, Pt and Au) and those elements with distribution coefficients between Fe-rich metal and silicate phases which exceed 10⁴. The large magnitude of these distribution coefficients makes them exceedingly difficult to measure experimentally. We describe a new experimental campaign aimed at obtaining reliable values of DMmets/sil melt for selected HSE's indirectly, by measuring the solubilities of the pure metals (or simple HSE alloys) in haplobasaltic melts as a function of oxygen fugacity.
dc.title	EXPERIMENTAL PETROCHEMISTRY OF SOME HIGHLY SIDEROPHILE ELEMENTS AT HIGH TEMPERATURES, AND SOME IMPLICATIONS FOR CORE FORMATION AND THE MANTLES EARLY HISTORY
dc.type	Статья

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