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(duì)柴西南盆地原型的形成與改造進(jìn)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(rèn)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(jī)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；