晚第三纪

wǎn dì sān jì
  • Late Tertiary;Neogene period
晚第三纪晚第三纪
晚第三纪[wǎn dì sān jì]
  1. 对研究区晚第三纪的古气候及成矿作用,也作了简要阐述。

    The paper has also brief reviewed on the paleoclimate and mineralization of Neogene period in the research area .

  2. 晚第三纪塔里木盆地及以南地区煤和盐类矿产沉积特征研究

    Research on Sedimentary Features of Coal and Halogen Minerals of Neogene Period in Tarim Basin and The South Area of It

  3. 晚第三纪的沉积厚度近似于E2末剥蚀厚度,对油气生成和运移的影响不大。

    The sedimentary thickness of Neogene is similar to that of denudation in the end of E 2 , which has only little influence on the formation and migration of oil and gas .

  4. 其后,季风系统在晚第三纪又经历了巨大变化,包括15~13Ma前、8Ma、3Ma前干旱气候的加剧和季风系统的加强。

    Since then , the Neogene has witnessed significant variations of the monsoon system , including enhancement of aridity and monsoon intensity at about 15 ~ 13 Ma , around 8 Ma and 3 Ma .

  5. 应用Easy-Ro(%)数值模拟方法对下白垩统烃源岩生烃史的研究表明,本区主要生油期为晚第三纪-第四纪,不存在二次生烃作用。

    Applying the Easy-Ro ( % ) model to the hydrocarbon generating history research of the lower Cretaceous source rocks shows that the main oil-generating period is from late Tertiary to Quaternary , and does not exist the second hydrocarbon-generating event during the geological time .

  6. 晚第三纪以来断裂活动微弱。

    The activity of the fault has been weak since Neogene .

  7. 晚第三纪以前形成古土壤的鉴别、分类及其在古环境研究中的应用

    Identification , Classification and Application in Paleoenvironment Research of Pre-Neogene Paleosols

  8. 滇西南晚第三纪含煤盆地的形成与演化

    Formation and evolution of late Tertiary coal-bearing basin in Southwest Yunnan

  9. 晚第三纪以来中国古环境的特征及其发展历史

    The characteristics and evolution of paleoenvironment of China since late Tertiary

  10. 晚第三纪武汉地区的化石木对当地古气侯的指相

    The late Tertiary climate in Wuhan area recognized by fossil woods

  11. 云贵高原首次发现晚第三纪海相化石&有孔虫

    First discovery of Neogene marine remains & foraminifera in the Yunnan-Guizhou Plateau

  12. 裂变径迹定龄法所确定的日本岛晚第三纪构造运动

    The tertiary geotectonic movement in Japanese Islands defined by fission track dating

  13. 火成岩活动主要集中在晚第三纪和第四纪。

    The activity of igneous rocks mainly concentrates in Neogene and Quaternary .

  14. 兰州地区晚第三纪地层的沉积相与古环境记录

    The Sedimentary Facies and Paleoenvironment Records of Late Tertiary in Lanzhou Area

  15. 黄河中游晚第三纪与第四纪古气候关系初探

    Preliminary Comparison of Paleoclimatic Characteristics in Quaternary and Late Neogene

  16. 郯庐断裂带晚第三纪以来的浅部挤压活动与深部过程

    Post-eogene compressive activities on the Tan-Lu fault zone and their deep processes

  17. 云南晚第三纪化石木研究及其古气候意义

    Neogene Fossil Woods of Yunnan Province and Their Palaeoclimate Implications

  18. 云南景谷盆地晚第三纪介形类

    Late Tertiary nonmarine OSTRACODS FROM Jinggu basin , yunnan

  19. 云南景谷盆地晚第三纪地层

    Late Tertiary Formation in Jinggu basin in Yunnan Province

  20. 云南中西部地区晚第三纪孢粉植物群及其古植被和古气候研究

    Palynology , Paleovegetation and Paleoclimate of Neogene Central - Western Yunnan , China

  21. 江苏南京地区晚第三纪植物

    Some Neogene plant fossils from Nanjing area , Jiangsu

  22. 崖19-1-1井晚第三纪浮游有孔虫深度分层及其古海洋学意义

    Depth stratification of late Tertiary planktonic foraminifera and their implications of well ya 19-1-1

  23. 三峡及邻区晚第三纪以来构造应力场特征探讨

    The features of recent tectonic stress field in Three Gorges and its neighbouring area

  24. 腾格里沙漠东南缘晚第三纪古风成砂及其环境

    Late Tertiary Eolian Sand Accumulation and Its Environment in the Southeastern Marginal Tengger Desert

  25. 晚第三纪以来油气藏调整为主阶段。

    The modification of pools dominated since Neogene .

  26. 江西晚第三纪地层的发现

    The discovery of late Tertiary strata in Jiangxi

  27. 兰州地区晚第三纪沉积序列的磁性地层与古环境意义

    The Study of Magnetostratigraphy and Paleoenvironment Evolution of Neogene Sedimentary Sequences in Lanzhou Area

  28. 江汉盆地东缘晚第三纪&早更新世的古环境

    A Study of Neogene-Early Pleistocene Epoch Ancient Environment at the Eastern Edge of Jianghan basin

  29. 自晚第三纪以来本区主要受北东&北东东向挤压应力场控制。

    The region under investigation was subjected to a strong NW-SE tension in Early Tertiary .

  30. 黄土高原红粘土序列与晚第三纪的气候事件

    Red clay sequences in Chinese Loess Plateau and recorded paleoclimate events of the late Tertiary