• Okinawa ocean trough and Ryukyu island arc were formed in late Miocene.

    中新世晚期冲绳疏球岛弧形成

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  • The timing of oil and gas migration are computed, it was late Miocene to Quaternary.

    认为珠三坳陷油气大量运移时期中新第四纪

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  • The climate aridity event of Late Miocene can be correlated with the global climatic event.

    本区中新世末期气候事件全球冷干气候事件一致。

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  • Miocene mammalian footprints have been recently identified from several Late Miocene localities in Iran.

    伊朗中新世的几个地点新近发现了哺乳动物足迹化石。

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  • The faulting might be attributed to the ascending lower crust-derived fluids after the Late Miocene epoch.

    造成断裂分期活动的原因是藏东地区地壳流体存在。

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  • The NNE_trending faults are relatively closed and the WNW_trending ones relatively opened during Late Miocene.

    中新世晚期,NNE向断裂相对封闭,WNW向断裂相对开启

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  • After Late Miocene, the basin got into a post_rift thermal subsidence stage in a shallow to semi_deep sea environment.

    中新世以后盆地进入浅海半深海沉积环境的裂后沉降

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  • This study notes that no reliable Late Oligocene to Miocene nannofossil markers were found in these 2 crusts. Furthermore, sedimentation hiatus was observed.

    研究注意2个结壳中没有发现可信的新世到中新世的化石记录,在个别层位之间存在着沉积间断

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  • During the period from Late Oligocene to Middle Miocene, the basin changed from rifting to depression, and the depositional area continued to expand in the Marine environment.

    渐新世—中新世盆地逐渐陷转为断拗,沉积范围不断扩大,整体处于海相沉积环境。

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  • Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary.

    包裹体分析表明,盆地油气运移始于渐新世—中新世,延续至第四纪。

    youdao

  • Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary.

    包裹体分析表明,盆地油气运移始于渐新世—中新世,延续至第四纪。

    youdao

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