Based on gravity and magnetic data the existence and boundary of palaeo - Junggar land were discussed.

依据重磁力和地壳厚度等资料,论述了准噶尔古陆片的存在及其边界,并认为其上有古生代的陆表海沉积.

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Basin basement palaeo - heat flow is a basic boundary parameter condition to realize basin geothermal field simulation.

盆地基底古热流是实现盆地地热场模拟的基础边界参数条件.

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This result has vital significance for in - depth basin analysis, palaeo - geomorphology resume and reservoir prediction.

研究成果对深入盆地分析 、 古地貌恢复、储层预测具有重要意义.

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