Kerogen is the leftover material of sporopollen element and lignin in original bodies in different thermal metamorphic period and it is the original material of gas-oil formation.

 
  • 干酪根主要是母源體中的孢粉素與木質(zhì)素在埋藏環(huán)境中不同熱變質(zhì)階段的殘留物,是油氣形成的母源物。
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