marginal-ocean basin 中文意思是什麼
marginal-ocean basin
解釋
邊緣洋盆-
The marginal ocean basin ' s formation and evolution model may be as follows : early triassic, rift was formed by extension and splitting in india ( gondwana ) continental margin during it was drifting southward ; late triassic, the rift had been joined in the neo - tethys ocean in the east and converted into initial ocean basin, and ayila - zhongba micro - continental was formed in north of the rift
洋盆的演化模式是:早三疊世,隨著印度(岡瓦納)大陸向南漂移,其北部邊緣因引張裂解產生裂谷,于晚三疊世向東開口與新特提斯洋主體連通,洋盆初具洋殼性質,北側形成阿依拉仲巴微陸塊。 -
Jurassic and cretaceous, the marginal ocean basin was in the stage of ocean crust evolution and had a setting similar to mid - ocean ridge
侏羅白堊紀為洋盆洋殼演化期,處于類似洋中脊的構造環境。 -
The authors put forward that daba - xiugugabu ophiolite belt originated from an ancient oceanic crust fragment of india continental northern marginal ocean basin, that was approximately synchronous with the formation and evolution period of the neo - tethys ocean
筆者提出該區蛇綠巖來源於印度大陸北緣洋盆的洋殼碎片,這個陸緣洋盆與新特提斯洋主體的形成和演化準同步。 -
During subduction northward of neo - tethys oceanic plate, ayla - zhongba micro - continental, the marginal ocean basin and india continental drifted northward all together, the marginal ocean basin was gradually contracted and closed by compressed of india continental
在新特提斯洋板塊向北俯沖消減過程中,阿依拉仲巴微陸塊、陸緣洋盆和印度大陸一起隨著向北漂移,在印度大陸向北擠壓作用下洋盆逐漸收縮以致最終閉合。
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