1.
Plio-Pleistocene paralic sands
上新世-更新世近海砂层
2.
Plio-Miocene beds
上新世-中新世地层
3.
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
4.
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
5.
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
6.
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
7.
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
8.
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。
9.
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
10.
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
11.
It intruded Eocene sandstones.
它侵入始新世砂岩。
12.
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
13.
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
14.
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
15.
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
16.
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
17.
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
18.
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