Result of analysis showed that the original organic matter was formed in lacustrine depositional environment with strong reduction and high salinity.There is also some carbonate source rocks as...

 
  • 分析結果表明油苗原始有機質(zhì)形成于強還原超鹽度的湖相沉積環(huán)境,部分生物標志化合物參數指示碳酸鹽巖生油巖的存在。
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