Last Updated：2025/11/28
During diagenesis, the sediments were pyritizing, which produced distinctive sulfur isotope signatures.
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During diagenesis, the sediments were pyritizing, which produced distinctive sulfur isotope signatures.
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成岩作用中に、堆積物は黄鉄鉱化しており、独特の硫黄同位体組成を示した。
