late-miocene

基本解釋

The faulting might be attributed to the ascending lower crust-derived fluids after the Late Miocene epoch.
造成斷裂分期活動(dòng)的原因是藏東地區(qū)下地殼流體的存在。
The super-pressure system of The Ya21-1 structure was formed during late Miocene, obviously earlier than the main stage of gas generation and expulsion of the source rock.
超壓的形成妨礙了天然氣的區(qū)域性運(yùn)移，是導(dǎo)致了崖21-1構(gòu)造未形成商業(yè)性氣田的主要原因。
The inversion from the Late Oligocene to the Middle Miocene led to obvious discrepancy of oil & gas accumulation between the northwestern and the central-southern parts of the basin.
晚漸新世—中中新世構(gòu)造反轉(zhuǎn)作用導(dǎo)致盆地西北部和中南部的油氣聚集特征存在明顯差異。

Phase One, the million and a half years ago, in the early--in the late--Miocene and early Pleistocene phases, there was shift where people were less likely to be just going out and gathering foods from every place they could find it.
第一階段,一百五十萬年前,在整個(gè)中新世以及更新世的早期,情況開始轉(zhuǎn)變,人們不光靠,出門四處搜集食物
耶魯公開課 - 關(guān)于食物的心理學(xué)、生物學(xué)和政治學(xué)課程節(jié)選