Breakdown of the source rock might be accelerated by biological mechanisms and by the high partial pressure of CO2 in soils.
岩石分解可以通过生物机制和土壤中部分高压二氧化碳得到加速。
Breakdown of the source rock might be accelerated by biological mechanisms and by the high partial pressure of CO2 in soils.
岩石分解可以通过生物机制和土壤中部分高压二氧化碳得到加速。
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