Qadam

基本解釋

There was much contention about the prototype of west-south Qadam basin because of its complex geology background.
摘要柴西南盆地原型的研究由於其複襍的地質(zhì)背景存在衆(zhòng)多爭論。
On the base of above named studies, the formation and reconstruction about the prototype of west-south Qadam were discussed.
以此爲(wèi)基礎(chǔ)，對柴西南盆地原型的形成與改造進行了探討。
The conclusions are as follows: Firstly, East Kunlun orogenic belt and west-south Qadam basin had suffered many periods of press and stretch events.
認爲(wèi)：中、新生代以來，東崑侖造山帶與柴西南盆地一起共同經(jīng)歷了多期擠壓與伸展事件。
Secondly, the pull-part geology background and the right-slip of Kunbei and Altun faults might be the main mechanism of prototype of Qadam basin during Cenozoic.
新生代早、中期的伸展環(huán)境及崑北斷裂、阿爾金斷裂的右行走滑可能是新生代柴西南原型盆地形成的主要機制。
Among them, East Kunlun orogenic belt underwent perhaps postorogenic stretch during Lower and Middle Jurassic that might be the direct cause of the prototype of west-south Qadam basin during Mesozoic.
其中，早、中侏羅世東崑侖山可能經(jīng)歷了造山後伸展事件，這一事件可能是中生代柴西南原型盆地的直接成因；