Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano

Svetlana G. Tessalina; Françoise Capmas; Jean-Louis Birck; Claude-Jean Allegre; Marina A. Yudovskaya; Vadirn V. Distler; Ilya V. Chaplygin

doi:10.1007/3-540-27946-6_214

Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano

Svetlana G. Tessalina^*, Françoise Capmas, Jean-Louis Birck, Claude-Jean Allegre, Marina A. Yudovskaya, Vadirn V. Distler, Ilya V. Chaplygin

^*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceeding › Conference proceeding contribution › peer-review

Abstract

Rhenium loss through magma degassing could be partly balanced by rhenium enrichment in fumarolic magmatic gases and Re-bearing precipitates, as may be the case for the Kudriavy volcano associated with an active subduction zone. The relatively unradiogenic (187)Os/(188)Os isotope ratios (0.122 up to 0.152) and high Os contents (averaging 0.6 ppb) of fumarolic gas condensates imply that significant Re and Os are remobilised from depleted MORB mantle. Involvement of a Re-rich component is evident from high Re concentrations in high-temperature gas condensates, ranging from 7 to 200 ppb. Indeed, Re-rich Os-poor components such as organic-rich subducted sediments and volcanic rocks do not significantly shift the isotopic composition of fumarolic products. The relatively radiogenic composition of the dacite-andesite-basaltic arc volcanics ((187)Os/(188)Os ratio up to 0.58), however, could result from significant Os (and Re) input from subducted sediments.

Original language	English
Title of host publication	Mineral deposit research
Subtitle of host publication	meeting the global challenge
Editors	Jingwen Mao, Frank P. Bierlein
Place of Publication	Berlin; Heidelberg
Publisher	Springer, Springer Nature
Pages	841-843
Number of pages	3
ISBN (Electronic)	9783540279464
ISBN (Print)	9783540279457
DOIs	https://doi.org/10.1007/3-540-27946-6_214
Publication status	Published - 2005
Externally published	Yes
Event	8th Biennial SGA Meeting - Beijing, China Duration: 18 Aug 2005 → 21 Aug 2005

Conference

Conference	8th Biennial SGA Meeting
Country/Territory	China
City	Beijing
Period	18/08/05 → 21/08/05

Keywords

Re-Os
subduction zone
rheniite
Kurile islands
Kudriavy
RE
SUBDUCTION
KUDRYAVY
ISLANDS
CRUST

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10.1007/3-540-27946-6_214

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Tessalina, S. G., Capmas, F., Birck, J.-L., Allegre, C.-J., Yudovskaya, M. A., Distler, V. V., & Chaplygin, I. V. (2005). Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano. In J. Mao, & F. P. Bierlein (Eds.), Mineral deposit research: meeting the global challenge (pp. 841-843). Springer, Springer Nature. https://doi.org/10.1007/3-540-27946-6_214

@inproceedings{f07f320ca9424592b93c868ddb1af64c,

title = "Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano",

abstract = "Rhenium loss through magma degassing could be partly balanced by rhenium enrichment in fumarolic magmatic gases and Re-bearing precipitates, as may be the case for the Kudriavy volcano associated with an active subduction zone. The relatively unradiogenic (187)Os/(188)Os isotope ratios (0.122 up to 0.152) and high Os contents (averaging 0.6 ppb) of fumarolic gas condensates imply that significant Re and Os are remobilised from depleted MORB mantle. Involvement of a Re-rich component is evident from high Re concentrations in high-temperature gas condensates, ranging from 7 to 200 ppb. Indeed, Re-rich Os-poor components such as organic-rich subducted sediments and volcanic rocks do not significantly shift the isotopic composition of fumarolic products. The relatively radiogenic composition of the dacite-andesite-basaltic arc volcanics ((187)Os/(188)Os ratio up to 0.58), however, could result from significant Os (and Re) input from subducted sediments.",

keywords = "Re-Os, subduction zone, rheniite, Kurile islands, Kudriavy, RE, SUBDUCTION, KUDRYAVY, ISLANDS, CRUST",

author = "Tessalina, {Svetlana G.} and Fran{\c c}oise Capmas and Jean-Louis Birck and Claude-Jean Allegre and Yudovskaya, {Marina A.} and Distler, {Vadirn V.} and Chaplygin, {Ilya V.}",

year = "2005",

doi = "10.1007/3-540-27946-6_214",

language = "English",

isbn = "9783540279457",

pages = "841--843",

editor = "Jingwen Mao and Bierlein, {Frank P.}",

booktitle = "Mineral deposit research",

publisher = "Springer, Springer Nature",

address = "United States",

note = "8th Biennial SGA Meeting ; Conference date: 18-08-2005 Through 21-08-2005",

}

Tessalina, SG, Capmas, F, Birck, J-L, Allegre, C-J, Yudovskaya, MA, Distler, VV & Chaplygin, IV 2005, Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano. in J Mao & FP Bierlein (eds), Mineral deposit research: meeting the global challenge. Springer, Springer Nature, Berlin; Heidelberg, pp. 841-843, 8th Biennial SGA Meeting, Beijing, China, 18/08/05. https://doi.org/10.1007/3-540-27946-6_214

Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano. / Tessalina, Svetlana G.; Capmas, Françoise; Birck, Jean-Louis et al.
Mineral deposit research: meeting the global challenge. ed. / Jingwen Mao; Frank P. Bierlein. Berlin; Heidelberg: Springer, Springer Nature, 2005. p. 841-843.

Research output: Chapter in Book/Report/Conference proceeding › Conference proceeding contribution › peer-review

TY - GEN

T1 - Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano

AU - Tessalina, Svetlana G.

AU - Capmas, Françoise

AU - Birck, Jean-Louis

AU - Allegre, Claude-Jean

AU - Yudovskaya, Marina A.

AU - Distler, Vadirn V.

AU - Chaplygin, Ilya V.

PY - 2005

Y1 - 2005

N2 - Rhenium loss through magma degassing could be partly balanced by rhenium enrichment in fumarolic magmatic gases and Re-bearing precipitates, as may be the case for the Kudriavy volcano associated with an active subduction zone. The relatively unradiogenic (187)Os/(188)Os isotope ratios (0.122 up to 0.152) and high Os contents (averaging 0.6 ppb) of fumarolic gas condensates imply that significant Re and Os are remobilised from depleted MORB mantle. Involvement of a Re-rich component is evident from high Re concentrations in high-temperature gas condensates, ranging from 7 to 200 ppb. Indeed, Re-rich Os-poor components such as organic-rich subducted sediments and volcanic rocks do not significantly shift the isotopic composition of fumarolic products. The relatively radiogenic composition of the dacite-andesite-basaltic arc volcanics ((187)Os/(188)Os ratio up to 0.58), however, could result from significant Os (and Re) input from subducted sediments.

AB - Rhenium loss through magma degassing could be partly balanced by rhenium enrichment in fumarolic magmatic gases and Re-bearing precipitates, as may be the case for the Kudriavy volcano associated with an active subduction zone. The relatively unradiogenic (187)Os/(188)Os isotope ratios (0.122 up to 0.152) and high Os contents (averaging 0.6 ppb) of fumarolic gas condensates imply that significant Re and Os are remobilised from depleted MORB mantle. Involvement of a Re-rich component is evident from high Re concentrations in high-temperature gas condensates, ranging from 7 to 200 ppb. Indeed, Re-rich Os-poor components such as organic-rich subducted sediments and volcanic rocks do not significantly shift the isotopic composition of fumarolic products. The relatively radiogenic composition of the dacite-andesite-basaltic arc volcanics ((187)Os/(188)Os ratio up to 0.58), however, could result from significant Os (and Re) input from subducted sediments.

KW - Re-Os

KW - subduction zone

KW - rheniite

KW - Kurile islands

KW - Kudriavy

KW - RE

KW - SUBDUCTION

KW - KUDRYAVY

KW - ISLANDS

KW - CRUST

U2 - 10.1007/3-540-27946-6_214

DO - 10.1007/3-540-27946-6_214

M3 - Conference proceeding contribution

SN - 9783540279457

SP - 841

EP - 843

BT - Mineral deposit research

A2 - Mao, Jingwen

A2 - Bierlein, Frank P.

PB - Springer, Springer Nature

CY - Berlin; Heidelberg

T2 - 8th Biennial SGA Meeting

Y2 - 18 August 2005 through 21 August 2005

ER -

Tessalina SG, Capmas F, Birck JL, Allegre CJ, Yudovskaya MA, Distler VV et al. Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano. In Mao J, Bierlein FP, editors, Mineral deposit research: meeting the global challenge. Berlin; Heidelberg: Springer, Springer Nature. 2005. p. 841-843 doi: 10.1007/3-540-27946-6_214

Sources of rhenium and osmium enrichment in fumaroles, sulphide sublimates and volcanic rocks from the Kudriavy volcano

Abstract

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Keywords

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