The tectonic evolution history of Tianshan is an example. In the Triassic, it was once uplifted to form the mountains with thick molasse accumulation on both its sides, Junggar and Tarim Basins. Then it became a peneplain by the exposion and deplanation in the Jurassic, forming the widespread coal-bearing strata which can be correlated. From the Cretaceous to the Early Cenozoic, it was uplifted again, until the Quaternary to build huge mountains with two large sedimentary basins on both sides.

如天山山脈的構(gòu)造演化久草网在线地址，三疊紀(jì)天山曾經(jīng)一度隆起成山，兩側(cè)的準(zhǔn)噶爾和塔里木盆地中堆積了巨厚的磨拉石免费黄色网址直接进入；侏羅紀(jì)時由於剝蝕夷平成為一個準(zhǔn)平原毛片在线观看免费网站，形成了廣泛分布且可以對比的含煤巖系；從白堊紀(jì)到早新生代欧美精品中文字幕在线视频，它再度隆升美女扒开腿让男人桶爽免费动态图，直至第四紀(jì)時形成雄偉的高大山系，兩側(cè)形成相應(yīng)的大型沈積盆地国产AAA免费黄色视频。

planation stream piracy：夷流襲奪

醫(yī)療泉 medicinal spring | 夷流襲奪 planation stream piracy | 夷平作用 deplanation

Ichang limestone：宜昌灰?guī)r(早奧陶紀(jì))

夷平作用 deplanation | 宜昌灰?guī)r(早奧陶紀(jì)) Ichang limestone | 移動波 wave of translation