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  1. 防災科研関係論文

Real-time drill mud gas logging at the USDP-4 drilling, Unzen volcano, Japan

https://nied-repo.bosai.go.jp/records/4310
https://nied-repo.bosai.go.jp/records/4310
3087872e-1b02-4a09-9e75-986eabc29e61
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Real-time drill mud gas logging at the USDP-4 drilling, Unzen volcano, Japan
言語
言語 eng
著者 Andreas Tretner

× Andreas Tretner

en Andreas Tretner

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Martin Zimmer

× Martin Zimmer

en Martin Zimmer

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Jörg Erzinger

× Jörg Erzinger

en Jörg Erzinger

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Setsuya Nakada

× Setsuya Nakada

en Setsuya Nakada

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Masaki Saito

× Masaki Saito

en Masaki Saito

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抄録
内容記述タイプ Other
内容記述 During the Unzen conduit drilling project USDP-4, the gas phase dissolved in the drill mud was continuously analyzed. Starting from the volcano's north flank an almost complete gas profile was achieved to the final depth of 1995.75 m in July 2004. Limitations were given due to the extremely difficult drilling conditions. The highly fractured rock formation led to loss of drill mud circulation in the shallow parts of the drill hole. Significant fluid inflow horizons did not occur above 800 m (drill string length). Starting from that depth on, invading fluids were detected with the real-time gas monitoring system. Major variations in the mud gas composition occurred only below a depth of 1000 m. Of major importance are fluid inflow zones with high 3He/4He at depths of 1555 m (7.3 RA), 1755.5 m (7.48 RA) and 1977.4 m (6.21 RA). These values indicate a significant influence of fluids with mantle signature. Furthermore, enhanced methane, radon and helium concentrations were also detected at specific depth. These detected major fluid- and gas inflow horizons may be able to explain magmatic degassing processes, related to the Unzen's eruption mechanism. This is generally true for the main fluid inflow zones and especially for the detected inflows at 1555 m, 1755.5 m and 1977.4 m. Furthermore, a correlation between lithology and gas composition was observed. Higher H2S concentrations were detected while drilling in pyrite-rich rocks. Cracks and fissures as well as lithological changes are often correlated with increasing amounts of gas. Trends with depth, from a minor to a more magmatic influenced regime were observed together with a change in hydrothermal alteration of the surrounding rock. This corresponds with the magmatic conduit zone which was penetrated at a depth of 1600 m, and supports the model of a high influence of hydrothermal fluid, accelerating cooling and mineral alteration. © 2008 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : Journal of Volcanology and Geothermal Research

巻 175, 号 1-2, p. 28-34
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0377-0273
DOI
関連識別子 10.1016/j.jvolgeores.2008.03.031
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