伊朗盆地是在中新生代受古特提斯洋与新特提斯洋的扩张闭合控制下形成的被动大陆盆地。
The Iran basin is a passive continental basin formed in Meso-Cenozoic under the control of the extensional closing of Paleotethys and Neo-tethys oceans.
晚侏罗世是龙门山前陆盆地演化的关键时期 ，因而沉积体系与古环境演化研究具有重要意义 。
The loesslike-palaeosoil series is one of the main bases for researching environment evolution of Holocene Epoch.
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