Helium isotope ratios of pore gases in deep-sea sediments, Leg 128

Y. Sano; M. Sakamoto; J. Ishibashi; H. Wakita; R. Matsumoto

doi:10.2973/odp.proc.sr.127128-1.182.1992

Helium isotope ratios of pore gases in deep-sea sediments, Leg 128

Y. Sano, M. Sakamoto, J. Ishibashi, H. Wakita, R. Matsumoto

Research output: Contribution to journal › Article › peer-review

9 Citations (Scopus)

Abstract

Helium in the samples can be explained by the mixing between atmospheric helium dissolved in bottom water of the Japan Sea and crustal helium in the sediment. The sedimentary helium is enriched in mantle-derived ³He compared with those from the Japan Trench and the Nankai Trough. This suggests that the basement of the Japan Sea has relatively large remnants of mantle-derived helium compared with that of the Pacific. Major chemical compositions of the samples are methane and nitrogen. There is a positive correlation between methane content and helium content corrected for air component. -from Authors

Original language	English
Pages (from-to)	747-751
Number of pages	5
Journal	Unknown Journal
DOIs	https://doi.org/10.2973/odp.proc.sr.127128-1.182.1992
Publication status	Published - 1992
Externally published	Yes

All Science Journal Classification (ASJC) codes

Environmental Science(all)
Earth and Planetary Sciences(all)

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10.2973/odp.proc.sr.127128-1.182.1992

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title = "Helium isotope ratios of pore gases in deep-sea sediments, Leg 128",

abstract = "Helium in the samples can be explained by the mixing between atmospheric helium dissolved in bottom water of the Japan Sea and crustal helium in the sediment. The sedimentary helium is enriched in mantle-derived 3He compared with those from the Japan Trench and the Nankai Trough. This suggests that the basement of the Japan Sea has relatively large remnants of mantle-derived helium compared with that of the Pacific. Major chemical compositions of the samples are methane and nitrogen. There is a positive correlation between methane content and helium content corrected for air component. -from Authors",

author = "Y. Sano and M. Sakamoto and J. Ishibashi and H. Wakita and R. Matsumoto",

year = "1992",

doi = "10.2973/odp.proc.sr.127128-1.182.1992",

language = "English",

pages = "747--751",

journal = "Unknown Journal",

issn = "1040-6182",

publisher = "Elsevier Limited",

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TY - JOUR

T1 - Helium isotope ratios of pore gases in deep-sea sediments, Leg 128

AU - Sano, Y.

AU - Sakamoto, M.

AU - Ishibashi, J.

AU - Wakita, H.

AU - Matsumoto, R.

PY - 1992

Y1 - 1992

N2 - Helium in the samples can be explained by the mixing between atmospheric helium dissolved in bottom water of the Japan Sea and crustal helium in the sediment. The sedimentary helium is enriched in mantle-derived 3He compared with those from the Japan Trench and the Nankai Trough. This suggests that the basement of the Japan Sea has relatively large remnants of mantle-derived helium compared with that of the Pacific. Major chemical compositions of the samples are methane and nitrogen. There is a positive correlation between methane content and helium content corrected for air component. -from Authors

AB - Helium in the samples can be explained by the mixing between atmospheric helium dissolved in bottom water of the Japan Sea and crustal helium in the sediment. The sedimentary helium is enriched in mantle-derived 3He compared with those from the Japan Trench and the Nankai Trough. This suggests that the basement of the Japan Sea has relatively large remnants of mantle-derived helium compared with that of the Pacific. Major chemical compositions of the samples are methane and nitrogen. There is a positive correlation between methane content and helium content corrected for air component. -from Authors

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U2 - 10.2973/odp.proc.sr.127128-1.182.1992

DO - 10.2973/odp.proc.sr.127128-1.182.1992

M3 - Article

AN - SCOPUS:0027100843

SN - 1040-6182

SP - 747

EP - 751

JO - Unknown Journal

JF - Unknown Journal

ER -

Helium isotope ratios of pore gases in deep-sea sediments, Leg 128

Abstract

All Science Journal Classification (ASJC) codes

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