miocene
miocene
1. BY THE END of the middle Miocene, roughly 13 million years ago, we have evidence for great apes in Eurasia, notably Lartet's fossil great ape, Dryopithecus, in Europe and Sivapithecus in Asia.
1300万年前，中新世中期结束，我们在欧亚大陆上找到了大猿化石，特别是拉特首先描述的欧洲大猿（林猿），以及亚洲的西瓦猿（Sivapithecus）。
2. LH4-1 Oilfield is a heavy oil field developed from the basis of the bioherm of Miocene Zhujiang Formation.
1油田是在新近系中新统珠江组生物礁基础上发育起来的稠油油田。
3. THIRD NOTE ON FOSSIL BIRD FROM MIOCENE OF LINQU, SHANDONG
三记山东临朐中新世的鸟化石
4. The second fold developed between late the Miocene and the initial stage of Early Pleistocene.
上新世晚期，早更新世初期，第二排褶皱开始形成。
5. There are a major source rock in coal measures of Eocene Pinghu Formation and a minor source rock in Oligocene and Miocene coal measures in the eastern depression belt.
东部坳陷带以始新统平湖组煤系地层为主要烃源岩。渐新统和中新统煤系地层为次要烃源岩。
6. The variation of the sandstone and conglomerate content in the Miocene to Pliocene regional cap rocks governed the types of the oil reservoirs and their oil contents.
中、上新统区域盖层中砂、砾岩含量的变化,控制济阳坳陷南、北方向上第三系地层油藏类型及其含油性的变化。
7. Post-rifting mainly occurred in Miocene and Pliocene and Quaternary, and formed Guantao，Minghuazhan and Pingyuan Formations.
中南区断陷走向呈近东西向、北东向和北西向，断陷都是北断南超的半地堑;
8. PALAEOECOLOGY OF AN EARLY-MIDDLE MIOCENE LAKE IN CHINA: PRELIMINARY INTERPRETATIONS BASED ON PHYTOLITHS FROM THE SHANWANG BASIN
中国-中新世湖泊的古生态:根据山旺盆地植硅体的初步解释
9. LAND MAMMAL FAUNAL SEQUENCE OF THE LATE MIOCENE OF CHINA: NEW EVIDENCE FROM LANTIAN, SHAANXI PROVINCE
中国晚中新世陆相哺乳动物群序列:陕西蓝田的新证据
10. The Miocene Epoch.
中新世
11. 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。
12. humid subtropical climate in the Miocene with temperatures higher than those of the Oligocene;
中新世为亚热带气候，气温比渐新世高；
13. CHANGES OF THE MONSOON-ARID ENVIRONMENT IN CHINA AND GROWTH OF THE TIBETAN PLATEAU SINCE THE MIOCENE
中新世以来我国季风-干旱环境演化与青藏高原的生长
14. About 3900 m thickness materials were denudated from the Red River drainage areas since Miocene.
中新世以来红河流域区被剥蚀掉约3900m。
15. North American cat of the Miocene and Pliocene; much earlier and less specialized than members of the genus Smiledon
中新世和上新世生活在美洲的猫科动物；对其研究也少
16. North American cat of the Miocene and Pliocene; much earlier and less specialized than members of the genus Smiledon.
中新世和上新世生活在美洲的猫科动物；对其研究也少。
17. good reservoirs are sandstones which include Miocene Letkat formation, Eocene Pondaung formation and Tilin formation.
中新世和渐新世砂岩为良好储层；
18. Trap character is not quite obvious in the Miocene, relatively larger in the Pliocene and weakenin the Pleistocene.
中新世圈闭特征并不十分明显，上新世形成的较大面积的构造圈闭，更新世圈闭特征减弱。
19. THE MIOCENE VEGETATION SUCCESSION AND ENVIRONMENTAL CHANGES IN SHANWANG BASIN, SHANDONG PROVINCE, CHINA
中新世山旺盆地植被演替与环境变迁
20. Early Miocene apes left Africa because of a new adaptation in their jaws and teeth that allowed them to exploit a diversity of ecological settings.
中新世早期，猿离开非洲，因为牠们的颚与牙齿演化出新的适应，使牠们能够利用各种不同的生态环境。
21. Miocene to the present time is the most active period for the post-fault thermal subsidence in China's offshore Tertiary basins.
中新世末至今是中国近海第三纪盆地裂后热沉降最活跃的时期,伴随着裂后构造再活动,断裂活动也十分活跃。
22. Volatiles from Two Gymnosperm Fossils: Miocene Leaves of Metasequoia glyptostroboides and Early Cretaceous Seed Cone of Pityostrobus spp.
中新世水杉叶片和白垩纪松型球果化石中的挥发性成分。
23. Miocene volcanic mechanism rocks
中新世火山岩
24. The deposits of the Miocene Epoch.
中新世的沉积物
25. GEOCHEMICAL CHARACTERISTICS OF THE MIOCENE EOLIAN DEPOSITS AND COMPARISON WITH THE PLIOCENE AND QUATERNARY EOLIAN DEPOSITS
中新世风尘堆积的地球化学特征及其与上新世和第四纪风尘堆积的比较
26. FIRST DISCOVERY OF MIOCENE BIRD IN CHINA
中新世鸟类在我国的首次发现
27. Eolian Sand Deposition and Its Environmental Significance in Linxia Basin Since Middle Miocene
临夏盆地晚中新世以来的风沙沉积及环境意义
28. To understand why the first apes were restricted in this way, consider the body plan of the early Miocene ape.
为什麽最早的猿在行动模式上受到那麽大的限制呢？
29. Fruits and Seeds from Yunnan in the Age of Miocene and from Shanxi in the Age of Pliocene
云南中新世和山西上新世果实和种子的研究
30. Late Miocene Woods of Taxodiaceae from Yunnan, China
云南中新世杉科化石木研究
31. A NEW SUID FROM THE UPPER MIOCENE HOMINOID LOCALITY IN YUANMOU OF YUNNAN PROVINCE
云南元谋含古猿地层猪科一新属
32. ANALYSIS ON THE HYDROCARBON-GENERATION CONDITIONS OF THE MIOCENE IN THE JINGGU BASIN, YUNNAN
云南景谷盆地中新统生油条件分析
33. SCIURIDS FROM THE LATE MIOCENE LUFENG HOMINOID LOCALITY, YUNNAN
云南禄丰古猿地点的松鼠类化石
34. From Paleocene to Miocene, the sedimentary facies evolved from the extensive alluvial fan to the braided fluvial river environment.
从古新世到中新世，柴达木盆地北缘经历了由大规模冲积扇沉积到辫状河沉积的演化过程。
35. The Eocene to Pliocene was generally wetter than today but increasingseasonality in rainfall led to the development of scleromorphy and xerophyfism fromabout the Miocene onwards.
从始新世到上新世，澳大利亚的气候总体上要比现在湿润，但降水量季节性变化的增强推动了中新世以后硬叶植物和旱生植物的发展。
36. From boundary to centre of the basin,the reservoir beds for exploring for gas are Oligocene,Miocene,Pliocene and Quaternary and the lithology changes from coarseness to fineness.
从盆地边缘到中心，有勘探意义的储层依次有渐新统、中新统、上新统和第四系，岩性由粗变细。
37. So the age of the Zhuhai Formation is assigned toOligocene, the age of the bottom of the Zhujiang Formation is also Oligocene, and therest of the Zhujiang Formation is Miocene.
从而判定珠海组时代为渐新世,珠江组底部时代也属于渐新世,珠江组下部的其余层段归属于中新世。
38. AFFINITIES AND IMPLICATIONS OF NEW MIOCENE MAMMAL FOOTPRINTS FROM IRAN
伊朗新发现的中新世哺乳动物足迹的亲缘关系及其意义
39. During the subduction, large-scale tectono-magmatic activities and epithermal Au mineralizations happened during the late Oligocene-middle Miocene.
俯冲过程中加里曼丹岛北缘在晚渐新世一中中新世发生大规模的构造岩浆活动及浅成低温热液金成矿作用。
40. So far 14 genera are known to have inhabited Africa during the early Miocene alone, between 22 million and 17 million years ago.
光是中新世早期（2200万到1700万年前），非洲至少就有14个属。
41. For decades, the prevailing hypothesis about Miocene Amazonia held that a shallow sea swamped the region for much of that epoch.
关于中新世的亚马逊河流域，过去数十年来，一般的假设是在中新世的绝大部份时间，有一座浅海淹没了该区。
42. Kuang, M.-Y.(1968) The lower Miocene gas reservoirs of the oil and gas fields in the Miaoli area, Taiwan. Petroleum Geology of Taiwan, 6, 157-182.
关明义(1968)苗栗地区诸油气田下部中新世储气层之研究。台湾石油地质，第6号，第157-182页。
43. Title： A NEW SPECIES OF PLATYBELODON (GOMPHOTHERIIDAE,PROBOSCIDEA, MAMMALIA) FROM EARLY MIOCENE OF THE DANGHE AREA, GANSU, CHINA
关键词：甘肃省党河地区,早中新世,嵌齿象科,铲齿象
44. A lot of enclaves named spinel lherzolite and pyroxenite derived from the mantle were fount in alkali basalt of Miocene Naitoushan period.
其中奶头山期碱性玄武岩中含有幔源的尖晶石二辉橄榄岩包体和辉石岩包体。
45. SPORO-POLLEN ASSEMBLAGE FROM THE MIOCENE TONGGUER FORMATION OF INNER MONGOLIA AND ITS CLIMATE
内蒙古中新统通古尔组孢粉组合及其气候
46. Discovery of Mantle Xenoliths Bearing Miocene Potassium-Rich Olivine Basalt and Its Significance in Siziwangqi Area, Inner Mongolia
内蒙古四子王旗东八号中新世含深源捕虏体富钾橄榄玄武岩的发现及其意义
47. ANCHITHERIUM FROM THE MIDDLE MIOCENE HALAMAGAI FORMATION OF NORTHERN JUNGGAR BASIN, XINJIANG
准噶尔盆地北缘哈拉玛盖组中的Anchitherium
48. Those correspond to Quaternary, Pliocene, Upper Miocene, Lower Miocene and Eocene respectively.
分别为第四系、上新统、中新统上段、中新统下段及始新统。
49. THE GRAIN SIZE EVIDENCES OF THE MIOCENE AEOLIAN SEDIMENTS AND ITS PALEOENVIRONMENTAL SIGNIFICANCE IN LINGYAN HILL, NANJING, EAST CHINA
南京灵岩山中新世风尘沉积的粒度证据与环境意义
50. Keywords Northern South China Sea;Strike-slip basin;Rift basin;Miocene marine source rock;Palaeogene continental source rock;
南海北部;走滑伸展型;断陷裂谷型;中新统海相烃源岩;古近系陆相烃源岩;
51. CARBONATE CONTENT CHANGES SINCE THE MIOCENE AND PALEOENVIRONMENTAL IMPLICATIONS, ODP SITE 1148, NORTHERN SOUTH CHINA SEA
南海北部ODP1148站中新世以来的碳酸盐含量变化及其古环境意义
52. LATE MIOCENE DIATOM RECORDS OF ODP SITE 1143 IN SOUTHERN SOUTH CHINA SEA
南海南部ODP1143站晚中新世沉积硅藻记录
53. Analysis of the subsidence history of the Zengmu basin in the southwest South China Sea since the early Miocene
南海西南部曾母盆地早中新世以来沉降史分析
54. A Pilot Study on Miocene through Holocene Sediments from the Continental Slope of the South China Sea in Correlation with Possible Distribution of Gas Hydrates
南海陆坡中新世以来沉积物特性与气体水合物分布初探
55. Researchers in southern South America have also made convincing cases that shallow marine conditions existed in inland Argentina during the Miocene.
南美洲南部的研究人员也提出了一些事实，让人相信在中新世时期，浅海的环境也存在于阿根廷内陆。
56. Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin,Qinghai
可可西里盆地中新统五道梁群湖相碳酸盐岩岩石学特征与沉积环境分析
57. The island arc-bearing areas of Taiwan, Luzon and Ryukyu are belts of seismic activity from the Miocene epoch.
台湾、吕宋和琉球等岛弧区是中新世以来地震多发区。
58. Yeh, M.-G. and Yang, J.Y.(1994) Depositional environments of the upper Miocene to Pleistocene series in the Chungpu area, Chiayi, Taiwan. Petroleum Geology of Taiwan, 29, 193-224.
叶明官、杨健一(1994)台湾嘉义中埔地区上部中新统至更新统沈积环境之研究。台湾石油地质，第29号，第193-224页。
59. It is proved that the Bottom Aquifer was composed of diluvial alluvial deposition and beds bearing gravel were mainly formed by rapid mud rock flow in fault basins during Miocene epoch when the paleoclimate was warm and dry.
各矿区的底含皆形成于气候干暖的新第三纪中新世 ,是一套在中、新生代断陷盆地内的山前洪积扇上由快速水流形成的洪积 -冲积物 ,含砾石地层多为泥石流沉积物
60. Yeh H. K., 1977. First discovery of Miocene bird in China. Vertebrata PalAsiatica, 15 (4): 244-248 (In Chinese with English abstract
周本雄,时墨庄,1978.山东临朐中中新世柄杯鹿头骨的发现,古脊椎动物与古人类,16(2):111-122
61. CHou, T.-H. Kuo, C.-L. Lin, L.-H. and Shen, J.-C. (1987) Hydrocarbons in the Miocene formations of northwestern Taiwan: a geochemical approach. Petroleum Geology of Taiwan, 23, 115-137.
周次雄、郭政隆、林丽华、沈俊卿(1987)台湾西北部中新统油气之地球化学研究。台湾石油地质，第23号，第115-137页。
62. Chou, J.-T.(1968) A stratigraphic and sedimentary analysis of the protoquartzite in the Miocene Talu Shale in northern Taiwan. Petroleum Geology of Taiwan, 6, 115-138.
周瑞炖(1968)台湾北部中新世打鹿页岩内砂岩之地层沉积研究。台湾石油地质，第6号，第115-138页。
63. Chou, J.-T.(1970) A stratigraphic and sedimentary analysis of the Miocene in northern Taiwan. Petroleum Geology of Taiwan, 7, 145-186.
周瑞炖(1970)台湾北部中新统之地层学及沈积学之研究。台湾石油地质，第7号，第145-189页。
64. Chou, J.-T.(1974) A sedimentologic and paleogeographic study of the Miocene Wuchihshan Formation in western Taiwan. Petroleum Geology of Taiwan, 11, 41-55.
周瑞炖(1974)台湾西部中新世五指山层之地层沈积及古地理之研究。台湾石油地质，第11号，第41-55页。
65. Chou, J.-T.(1975) A sedimentologic study of the Miocene Pachangchi Sandstone in the Chiayi region, western Taiwan. Petroleum Geology of Taiwan, 12, 81-96.
周瑞炖(1975)台湾西部嘉义区中新世八掌溪砂岩之地层沈积之研究。台湾石油地质，第12号，第81-96页。
66. Chou, J.-T.(1976) Sedimentology and paleogeography of the Miocene clastic sequence in northern Taiwan, with emphasis on its sandstones. Petroleum Geology of Taiwan, 13, 83-118.
周瑞炖(1976)台湾北部中新统之沈积学及其古地理注重于砂岩之研究。台湾石油地质，第13号，第83-118页。
67. Chou, J.-T.(1976) A sedimentologic and paleogeographic study of the Miocene Shihti Formation in western Taiwan. Petroleum Geology of Taiwan, 13, 119-138.
周瑞炖(1976)台湾西部中新世石底层之地层沈积及其古地理之研究。台湾石油地质，第13号，第119-138页。
68. Chou, J.-T.(1980) Stratigraphy and sedimentology of the Miocene in western Taiwan. Petroleum Geology of Taiwan, 17, 33-52.
周瑞炖(1980)台湾西部中新统之地层学及堆积学研究。台湾石油地质，第17号，第33-52页。
69. The oil source of oilsand in northern Kashi sag came from Jurassic hydrocarbon source whose reservoir-forming stage might be from Miocene to Pliocene.
喀什凹陷北部油砂的油源来自于侏罗系烃源岩，成藏期为中新世至上新世。
70. Since the Miocene Yanqi basin has been overthrusted from north by Tianshan belt and from south by Kuluktag belt because of the Himalayan orogenic event.The Yanqi basin is now one of foreland basins.
喜马拉雅造山事件以来，其南北两侧山体向盆地内对冲，形成典型前陆冲断褶皱构造，盆地内发育一系列台阶状断层及其断层相关褶皱。
71. Therefore, the existence of the late Cenozoic aeolian deposit demonstrates that the middle and west parts of the Tibetan Plateau have been dry since the middle Miocene time.
因此，中中新世以来湟水流域风尘堆积物的存在可能表明了青藏高原中西部在那时已经较为干旱。
72. In Qingyang, Gansu, Wudu late Miocene strata, etc., with the ancient symbiotic giraffe lips are big rhinoceros, rhinoceros Bandicota, Hipparion fossils and other ancient animals.
在庆阳、临夏、武都等晚中新世地层中，与古长颈鹿共生的还有大唇犀、板齿犀、三趾马等古动物化石。
73. With the same geological structural settings, the Miocene sequence development of the Shanwang,Baojiahe,and Qingshan Basins are comparable.
在相同构造背景下，山旺盆地、包家河盆地和青山盆地的中新世对应层位的层序发育特征具有可比性。
74. For the shallow traps in Yinggehai Formation, the main reason for episodic injection of fluid a with different gas components is the matching of trap formation and hydrocarbon generation in Miocene.
在莺歌海组浅层底辟圈闭中，圈闭形成期与中新统气源岩生烃过程的匹配是造成含不同天然气组分的流体发生幕式充注的主要原因。
75. E.Johnson et al.: The Late Miocene radiation of Modern Felidae: A genetic assessment.
基因研究对猫科的分类提出了一个更精确的分类法refW.
76. The Kekeya condensate oil and gas field in Tarim basin, where Upper and Lower Miocene oil formations, and the deeper Eocene oil formation developed, consists of seven condensate pools.
塔里木盆地柯克亚凝析油气田主要发育中新统上、下油组及始新统深部油组，由7个凝析油气藏组成。
77. Braided-river deltaic sediments of the Miocene Anju'an Formation in the Southwest depression, Tarim basin
塔里木盆地西南坳陷中新统安居安组辫状河三角洲沉积
78. a large extinct ground sloth of the family Megatheriidae of the Miocene Epoch through the Pleistocene 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
79. Eocene through lower Oligocene lacustrine shales and Oligocene through lower Miocene lacustrine and deltaic coaly shales are the mature source rocks.
始新世到渐新世湖泊页岩、渐新世到中新世到湖泊和三角洲页岩都是成熟的矿源岩。
80. Manius, William G.Covey, M.-C. and Stallard, Robert(1985) The effects of provenance and diagenesis on clay content and crystallinity in Miocene through Pleistocene deposits, southwestern Taiwan.
孟威廉、柯慕恺、史鲁柏(1985)来源地区与成岩作用对台湾西南部中新世至更新世沈积物中黏土含量与结晶度之影响。
