利用碳同位素、生物标记化合物、成熟度特征对比认为南带沥青显示分别来自下志留-中上奥陶统、中上寒武统、下寒武统和震旦系三套同位素分布有异的源岩；

利用碳同位素、生物标记化合物、成熟度特征对比认为南带沥青显示分别来自下志留-中上奥陶统、中上寒武统、下寒武统和震旦系三套同位素分布有异的源岩；的英文翻译

基本释义

• Using carbon isotopes and organism sign compound and character of maturity to compare, we think that asphaltum show in south cincture is from three set source rock of different carbon isotopes-lower Silurian to middle and upper Ordovician, middle and upper Cambrian lower Cambrian & Sinian;