博格达山属于晚古生代的陆间裂谷。
博格达山北缘以二叠系芦草沟组湖相油页岩为主要烃源岩。
The main hydrocarbon source rock in the The northern border of Bogd .
博格达山北麓油页岩资源储量巨大且发现已久，但研究程度较低。
The huge reserves of oil shale were detected long time ago at the northern foot of the Bogeda Mountain, but unfortunately, their research degree is relatively low.
博格达山北缘的石炭系柳树沟组岩层为准噶尔南缘东段前缘坳陷的主要物源。
The carboniferous Liushugou Formation in the northern area of the Bogda Mountain was the main source area of frontal depression.
而上苍房沟群以混杂物源区为特征，表明早三叠世隆升的博格达山已成为其物源区。
The upper Cangfanggou Group is with mixed characteristics of the source area and something shows that early Triassic swelling Bogda Mountain has become the source area.
这种差异性的隆升可能一方面与印度板块和欧亚板块碰撞的远程效应有关，另一方面也是更主要的原因可能受博格达山不同段深部差异性动力学过程所控制。
The difference in the uplifting may be because of collision between the Indian and Eurasian plates and also of being controlled by the processes of dynamics at different depths of Bogeda Mountain.
这种差异性的隆升可能一方面与印度板块和欧亚板块碰撞的远程效应有关，另一方面也是更主要的原因可能受博格达山不同段深部差异性动力学过程所控制。
The difference in the uplifting may be because of collision between the Indian and Eurasian plates and also of being controlled by the processes of dynamics at different depths of Bogeda Mountain.
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