craton basin 中文意思是什麼
craton basin
解釋
克拉通盆地-
The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton, and had experienced three period process of orogeny, including hercynian folding orogeny in continental margin, mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny, and late yanshanian to early himalayaian intracontinental range - basin post orogeny
認為阜新地塊是在克拉通裂陷槽基礎上發育起來的，經歷了海西期陸緣褶皺始造山、印支?早燕山陸內褶斷主造山、晚燕山?早喜馬拉雅陸內盆山後（重）造山等過程。 -
The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin, and shangrao and mingxi basins are the continental margin fault basins in the early triassic
早三疊世的中下揚子混積盆地屬克拉通邊緣盆地，而上饒和明溪碎屑巖盆地則為大陸邊緣斷陷盆地。 -
Ordos basin is known occurring on the stable north china craton, and there are relatively faint tectonic events in the inner of the basin, it is therefore important to make sedimentary facies and sequence stratigraphy research in order to clarify the distribution of reservoirs and explore oil and gas abundance areas
眾所周知，鄂爾多斯盆地發育于華北克拉通穩定基底之上，盆地內部構造活動比較微弱，因此，開展盆地沉積相與層序地層學研究，對于搞清儲集空間的展布規律、尋找油氣的富集區都具有十分重要的作用。 -
Ore - formation of basin fluids in the northern margin of north china craton - case studies
華北克拉通北緣與盆地流體有關的若干礦床實例 -
On the basis of analysis on the characteristics of structural evolution, the growth of the source rocks is analyzed. in the period of mesozoic - palaeozoic, caledonian events and the evolution of hercynian - early indo - chinese cycle are experienced in two - phase marine passive continental margin and craton basin in the lower and middle yangtze region, by which stable enormous thick mesozoic - palaeozoic deposites are induced, six sets of source rocks are produced, it has a strong capacity of hydrocarbon generation
摘要通過構造演化特徵分析了海相烴源巖的發育，中、下揚子區中古生代經歷了加里東和海西早印支旋迴兩個階段的海相被動大陸邊緣和克拉通盆地演化，形成了巖性穩定的巨厚中古生界，發育了6套烴源巖，具有較強的生烴能力。
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