The structural and thermal evolution of Hami depression, Taibei depression and Tuokexun depressions is very different.

吐哈盆地哈密坳陷 、 台北凹陷、托克逊凹陷构造热演化史差异较大.

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The Upper Palaeozoic source rocks in Jiyuan - Zhongmou - Huangkou depression belt experienced complicate structural and thermal evolution.

济源 - 中牟 - 黄口坳陷带的上古生界烃源岩经历了复杂的构造热演化历史.

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Knowledge on thermal evolution stages of Mesozoic strata in the Hefei basin is limited.

合肥盆地中生界地层的热演化程度以往了解的十分有限.

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