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。
The result shows that there were two different fluid flow areas in "Sanjiang" middle belt during Neo Tethys.
研究表明，三江中段新特提斯阶段区域流体存在两个性质不同的流体作用区域。
The result shows that there were two different fluid flow areas in "Sanjiang" middle belt during Neo Tethys.
研究表明，三江中段新特提斯阶段区域流体存在两个性质不同的流体作用区域。
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