The provenance for the turbidite might be located to the northeast of the studied area,evidenced by the vector structures such as sole cast structure in the turbidite.
根据底部印模构造指向,物源区大致位于研究区的北东。
参考来源 - 鄂尔多斯盆地东南部三叠系延长组一段湖相浊积岩特征及意义·2,447,543篇论文数据，部分数据来源于NoteExpress
基性火山岩系具有同一岩浆源区。
造成断流的主要根源是源区水资源的贫乏和湖面的蒸发。
Among which, shortages of water resource and lake surface evaporation are the major reasons.
管胞长度的种源区和产地效应很小，无一定的地理变异趋势。
There were very small effect of seed source and no definite geographic pattern in tracheid length.
应用推荐