دورية أكاديمية
Methane genesis within olivine-hosted fluid inclusions in dolomitic marble of the Hida Belt, Japan
العنوان: | Methane genesis within olivine-hosted fluid inclusions in dolomitic marble of the Hida Belt, Japan |
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المؤلفون: | Hironobu Harada, Tatsuki Tsujimori |
المصدر: | Progress in Earth and Planetary Science, Vol 11, Iss 1, Pp 1-13 (2024) |
بيانات النشر: | SpringerOpen, 2024. |
سنة النشر: | 2024 |
المجموعة: | LCC:Geography. Anthropology. Recreation LCC:Geology |
مصطلحات موضوعية: | Dolomitic marble, Fluid inclusion, Olivine, Abiotic methane synthesis, Hida Belt, Geography. Anthropology. Recreation, Geology, QE1-996.5 |
الوصف: | Abstract Abiotic synthesis of hydrocarbon-bearing fluids during geological processes has a significant impact on the evolution of both the Earth's biosphere and the solid Earth. Aqueous alteration of ultramafic rocks, i.e., serpentinization, which forms serpentinite, is one of the geological processes generating abiotic methane (CH4). However, abiotic CH4 generation is not limited to the serpentinization of mafic and ultramafic lithologies. Metasedimentary dolomitic marble from the Hida Belt, Japan, is characterized by the presence of forsterite-rich olivine (Fo~89–93), and olivine crystals contain abundant fluid inclusions ( |
نوع الوثيقة: | article |
وصف الملف: | electronic resource |
اللغة: | English |
تدمد: | 2197-4284 |
Relation: | https://doaj.org/toc/2197-4284 |
DOI: | 10.1186/s40645-024-00609-y |
URL الوصول: | https://doaj.org/article/4cc357866fa24c42bacbd39f09f3895d |
رقم الأكسشن: | edsdoj.4cc357866fa24c42bacbd39f09f3895d |
قاعدة البيانات: | Directory of Open Access Journals |
تدمد: | 21974284 |
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DOI: | 10.1186/s40645-024-00609-y |