The study shows that source rocks with a high level of organic matter abundance ( C ) but a bad kerogen type index ( KTI ) and those with a low level of C but a good KTI can both cross threshold of hydrocarbon expulsion .
研究表明,C(母质丰度)值高但KTI(母质类型指数)值低的烃源岩与C值低但KTI值高的烃源岩均能进入排烃门限;