miocene

Xunhua Basin section of pollen records reveal in the late Oligocene-Miocene in general represent a northeastern warm, temperate deciduous broad-leaved coniferous forest-temperate mixed forest-coniferous forest and arid mountain desert steppe vegetation landscape evolution.

循化剖面孢粉记录的研究揭示出循化地区在渐新世末期上新世早期总体上代表一种暖温带、温带落叶、阔叶针叶林温带针阔叶混交林山地针叶林与干旱草原荒漠的植被生态景观演变过程。

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Taking Luntai fault belt of northern Tarim uplift as an example, the main negative inversion phase of the fault may be Suwiyi-Jidike epoch of Miocene, and the inversion ratio is0.85~ 0.98.

对塔里木盆地北部隆起轮台断裂带进行的实例分析表明，轮台负反转断裂主反转期为中新世苏维依期一吉迪克期，反转率为0.85～0.98。

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The volcano of Changbaishan Tianchi had erupted many times since the Miocene with heavy disaster.

长白山天池火山是中新世以来多次喷发并造成严重灾害的火山。

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Sequence V is Miocene swamp variegated silt, mudstone interbedded by coaly shale and coal seam. The Oligocene middle grain silt probably deposited in the bottom.

层序V，为中新统沼泽相的杂色砂泥岩夹炭质页岩、煤层，往下可能还含有少量渐新统中细砂岩。

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Intense thrusting from Miocene controlled the formation of north foreland basins.

中新世以来的强烈冲断，控制了其北侧前陆盆地的形成。

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There are four hydrocarbon source rocks, Palaeocene, Eocene, Oligocene and Miocene.

西湖凹陷发育古新统 、 始新统 、 渐新统及中新统四大烃源岩系.

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Results show that northern temperate grassland came into being in Miocene ( about 7 to 10 million years ago) and strenuous evolution happened to ecological environment of grassland during the thousands years of human action.

研究表明北方温带草原形成于中新世末（约距今700&1000万年前），草原的生态环境在过去有人类活动的几千年间曾有过剧烈的变化。

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One of the most noticeable features of the Middle Miocene rock layers was their periodicity.

中新世中期的岩层,最显著的特徵之一,就是这些岩石所呈现的周期性.

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The Miocene sedimentation was terminated at about Messinian time due to the regional tectonic activities.

受区域构造活动的影响，大约在Messinian时结束了沉积作用。

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Great Barrier Reef was formed in the Miocene period, 2500 years have elapsed since the historical.

大堡礁形成于中新世时期, 距今已有2500万年的历史.

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In Late Cretaceous, Antarctica moved southwards and to the present position in Early Miocene.

白垩纪晚期，南极大陆向南移动，并于中新世早期到达现在位置。

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A porcupine from late Miocene of Linxia basin, gansu, China

甘肃临夏盆地晚中新世豪猪一新种

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Miocene foraminifera of Tarim basin, Xinjiang and their geological significance

新疆塔里木盆地中新世有孔虫及其地质意义

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It is suggested that Miocene ( 12Ma) can be defined as a borderline to mark off the two stages of Tertiary structural evolution, one is sliding and separate basin ( left-revolving) and the other is compressive and twisty depression basin ( right-revolving).

阐明了柴西第三系构造演化以中新统（12Ma）为界，可划分为走滑拉分盆地（左旋）与压扭坳陷盆地（右旋）两个主要阶段。

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Many turbidite sandstone bodies, deposited during the Middle Miocene to Pliocene, are distributed and form one of major reservoirs for oil and gas in the Tertiary Niigata backarc sedimentary basin, the most productive oil basin in the Japanese Islands.

沉积于中中新世到上新世的浊积砂体是第三纪Niigata弧后盆地的主要油气储层之一，该盆地是日本列岛最富产石油的盆地。

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Evolution of Ore-forming Condition of Co-rich Crusts From Lamont Guyot in the Western Pacific Since the Miocene

西太平洋Lamont海山中新世以来富钴结壳成矿环境的演化

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First Evidence of Sequoia in the Miocene of Yunnan Province, China

红杉属植物在中国云南中新世首次发现

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Ever since the Miocene time, aeolian dust has been falling down over Northwestern China, forming the Loess Plateau.

中国西北地区，从中新世以来就有持续不断的风尘沉积。

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The boundary between the Neogene/ Palaeogene Formation is located at the bottom of the N4 zone containing forams. The age of Zhuhai Formation defined by Nanhai East Corporation is Early Miocene.

上/下第三系界线置于浮游有孔虫N4带的底较为合适，南海东部公司目前所定义的珠海组的时代应归于早中新世；

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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.

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Eocene lavas belong to high K Calc alkaline ( HK CA) series and those of Miocene to shoshonite ( SHO) series.

渐新世火山岩为高钾钙碱性系列，中新世岩石属于钾玄岩系。

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The Middle and the South segments as the end of Miocene intermediate-acidic intrusive rocks.

南段以中新世末的中酸性侵入岩为主；

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The Miocene Sedimentation in the Reggio di Calabria, South Italy

意大利南部雷焦卡拉布里亚地区中新世沉积作用

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A large extinct ground sloth of the family Megatheriidae of the Miocene Epoch through the Epoch.

大懒兽中新世至更新世时期大懒兽科之栖于地面的已绝迹的大树懒.

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Subaqueous tidal delta of Zhujiang basin in the early lower Miocene

珠江口盆地下中新早期的水下潮汐三角洲

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Chinese Officials and Ryukyu 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。

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The climate difference between the early middle Miocene Shanwang palaeoclimate and the present day climate of the Shanwang region are mainly associated with significantly reduced levels of precipitation ( mean annual precipitation and rainfall distribution) and much colder mean temperatures in the coldest month.

与现代山旺地区气候上的区别主要在于年平均降雨量、降雨量的分配，以及最冷月份的平均温度。

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Miocene formations ( better: strata ) are well-exposed in this area.

本区具有出露良好的中新世地层.

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Fault chronology and sedimentation of the downfaulted basins indicate that extensional deformation in the study region was initiated in the late Miocene to early Pliocene at least, which has had a marked controlling effect on the present geomorphologic framework and drainage pattern in the region.

断层年代学和断陷盆地沉积作用研究结果表明，研究区伸展变形至少自中新世末&上新世初就已开始，对长江源地区现今的地貌格局、水系型式具有显著的制约作用。

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Miocene fossils from Okinawa Trough and their Stratigraphical Significance the stratigraphical division of DC-2 columnar core from the East China Sea

冲绳海槽海底中新世化石的发现及其地层意义东海DC-2孔柱状岩芯的地层划分

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