摘要
国内外勘探实践表明,大型可燃有机矿田都分布在一定的构造部位。这种构造部位主要就是斜交的两构造带或两断裂带所围限的基底沉降地段,称构造交角区。 构造交角区有其独特的沉积建造、地质构造特征和复杂的发育历史,其规律性相当明显。认识这些规律和特征,对勘探和开发新疆的可燃有机矿产当有裨益。
Basement-depressed areas bounded by two intersecting tectonic belts or fault zones are commonly settings in which aboundent combustible organic mineral resources occur. Such tectonic units are referred to as tectonic angle areas by the author of this paper. A study of the tectonic angle areas in terms of their control of the occurrences of combustible organic deposits is presented and it is of both theoretical significance and economic value in exploring for further such deposits.
出处
《新疆地质》
CAS
1985年第4期19-28,共10页
Xinjiang Geology
