Okinawa ocean trough and Ryukyu island arc were formed in late Miocene.
中新世晚期，冲绳海槽和疏球岛弧形成。
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的时期为晚中新世到第四纪。
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与全球冷干气候事件一致。
Miocene mammalian footprints have been recently identified from several Late Miocene localities in Iran.
伊朗晚中新世的几个地点新近发现了哺乳动物足迹化石。
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下地壳流体的存在。
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。
After Late Miocene, the basin got into a post_rift thermal subsidence stage in a shallow to semi_deep sea environment.
晚中新世以后，盆地进入浅海半深海沉积环境的裂后热沉降期。
This study notes that no reliable Late Oligocene to Miocene nannofossil markers were found in these 2 crusts. Furthermore, sedimentation hiatus was observed.
研究注意到在2个结壳中都没有发现可信的晚渐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。
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.
晚渐新世—中中新世，盆地逐渐由断陷转为断拗，沉积范围不断扩大，整体处于海相沉积环境。
Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary.
包裹体等分析表明，盆地油气运移始于晚渐新世—早中新世，延续至第四纪。
Inclusion data shows that the migration of petroleum in the basin initiated from the Late Oligocene to the Early Miocene, up to the Quaternary.
包裹体等分析表明，盆地油气运移始于晚渐新世—早中新世，延续至第四纪。
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