دورية أكاديمية

Methane genesis within olivine-hosted fluid inclusions in dolomitic marble of the Hida Belt, Japan

التفاصيل البيبلوغرافية
العنوان: Methane genesis within olivine-hosted fluid inclusions in dolomitic marble of the Hida Belt, Japan
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
الوصف
تدمد:21974284
DOI:10.1186/s40645-024-00609-y