pliocene pleistocene boundary

基本解释上新世更新世边界

网络释义

1)pliocene pleistocene boundary,上新世更新世边界2)Plio-Pleistocene,上新世/更新世3)Pliocene-Pleistocene,上新世-早更新世4)Plio-Pleistocene paralic sands,上新世-更新世近海砂层5)late pleistocene,晚更新世6)pleistocene epoch,更新世

用法和例句

This paper links sedimentary petrology with structural geology, so is the other branch subjects, penetrates into researching the Pliocene-Pleistocene sediments of t.

大邑砾岩的地质时限为上新世-早更新世,时代界定在4。

Characteristics of Palynological Assemblage of Late Stage of Late Pleistocene in Changjiang River Delta Area and Paleoenvironment;

长江三角洲地区晚更新世晚期的孢粉特征及古环境

The Sporopollen Assemblages and Their Paleoenvironment Significance of the Qianhu Bay,Zhangpu,Fujian since Late Pleistocene;

福建漳浦前湖湾晚更新世的孢粉组合及其古环境意义

The distribution of elephant fossils and the physiognomy characters of late Pleistocene in Jixian County of Tianjin;

天津蓟县晚更新世象化石分布与地貌特征

Investigation on Split Trace of Mammal Bone Fossils of Pleistocene Epoch from Western Hunan;

湘西更新世哺乳动物化石痕迹考察研究

The climate in Pleistocene epoch in Henan changed from burning hot multi-rain tropics or the subtropics climate to half drought and drought climate.

河南更新世时期的气候,是由炎热多雨的热带或亚热带气候向半干旱、干旱气候转变的,在这一转变过程中,有多次温暖气候与寒温气候的更迭。

Plio-Pleistocene paralic sands

上新世-更新世近海砂层

Plio-Miocene beds

上新世-中新世地层

LATE PLIOCENE CHANGES OF UPPER OCEAN STRUCTURE IN THE SOUTHERN SOUTH CHINA SEA

南沙海区晚上新世海水上层结构变化

Sequence Stratigraphy of Pliocene-Eopleistocene Epoch and Its Paleoenvironmental Significance in Zanda Basin, Tibet;

西藏札达盆地上新世—早更新世层序地层学及其古环境意义

Chemical Element Distribution and Palaeoclimate in Late Pleistocene-Holocene Strata in East Gonghe Basin

青海共和盆地东部晚更新世——全新世地层中元素分布与古气候

FEATURES OF PLIOCENE STRATA AND LITHOSTRATIGRAPHIC UNITS ON HAINAN ISLAND

海南岛上新世地层特征及岩石地层单位

The State Concept Held in Shanghai s Intellectuals at early Twentieth Century;

20世纪初年上海知识界国家观念的更新

The eastern Yantai-Weihai segment is a mid Pleistocene segment on which no late Pleistocene offset has been found.

东段烟台威海段为中更新世活动段,没有发现晚更新世地层错断现象。

Paleoenvironment Evolution in the Okinawa Trough During the Late Pleistocene and Holocene;

冲绳海槽晚更新世——全新世的古环境演化

The Discovery of Palaeo-eolian Sand and Environmental Changes of the Late Pleistocene in Lanzhou Area

兰州地区晚更新世古风成砂的发现及环境变化

It intruded Eocene sandstones.

它侵入始新世砂岩。

Palynological Assemblage and Correlation of Climate Stratigraphy Since Holocene in the Changjiang River Estuary and Its Approach of the Southern Yellow Sea;

长江口及邻近海域全新世以来孢粉组合及气候地层对比

The Pliocene Nannofossil Assemblages and Variation of the Upper Ocean Structure from ODP1146 in the Northern South China Sea;

南海北部ODP1146站位上新世超微化石组合及上层海水结构变化

Open up New Prospect of Oceanic and Fisheries in LiaoningProvince at Beginning of New Century;

努力开创新世纪“海上辽宁”建设新局面

Urban Renewal and Sustainable Development: on Issues of Shanghai Urban Development towards 21th Century

城市更新与城市持续发展──兼论21世纪上海城市建设中的几个问题

Further Research in the Development of the MarineIndustry in Shanghai;

推进上海新世纪海洋产业发展的研究

THE SEDIMENTARY STRUCTURES AND THE FACIES MODEL OF THE LATE PLEISTOCENE EOLIAN BIOCALCARENITES IN SHIDAO ISLAND OF XISHA ARCHIPELAGO

西沙石岛晚更新世风成生物砂屑灰岩的沉积构造和相模式

THE EXISTENCE OF MARINE EOCENE STRATA FROM THE EAST CHINA SEA BASIN AND ITS SIGNIFICANCE

东海盆地海相始新世地层的存在及其意义

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