博格达山属于晚古生代的陆间裂谷。
现在博格达什维斯基在为几个国外富翁做心理训练。
And now, Bogdashevsky is training the psyches of a couple of wealthy foreigners.
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 .
博格达山前褶皱带是我国最复杂、最雄伟的山前构造单元之一。
Pre—Bogda mountain folded zone is one of the most complicate and grand tectonic unit at pre—mountain area in China.
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.
“抛掉负面情绪，”翻译转述博格达什维斯基的话，“给你们的耳朵热身一下！”
"Throw away negative emotion," the translator says as Bogdashevsky rubs his ears. "Warm up your ears!"
天池是一个高山湖泊，居海平面以上，位于博格达峰北部一千九百一十米处的峡谷内。
And that Heavenly lake was a high-mountain lake located in a valley on the northern part of Bogda Peak 1910 meters above sea level.
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.
以博格达地史演化为主线，探讨博格达构造域成盆—成烃—成藏的演化过程。
Based on the geological history evolution of Bogda, in this paper the process of basin formation, hydrocarbon generation and petroleum accumulation of Bogda region are discussed.
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.
晚期开始出现分异，表现为博格达山南坡及柴窝铺地区沉积物扩散方向转为北北东向。
At the late phrase, the deposit spreading direction of the south slope in the Bogda Mt. and Chaiwopu area shift to the direction of north north-east.
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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