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.
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。
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The evolutionary tendance reflected by the above sedimentary record probably signifies an important tectonic turn in the history of the residual Paleotethys ocean.