Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 23 Issue 1
Feb.  2012
Turn off MathJax
Article Contents

Yuri D, Olga P, Alexander M, Tatiana A, Tamara B, Kazushige Tanabe, Yasunari Shigeta, Haruyoshi Maeda. Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido. Journal of Earth Science, 2012, 23(1). doi: 10.1007/s12583-012-0230-0
Citation: Yuri D, Olga P, Alexander M, Tatiana A, Tamara B, Kazushige Tanabe, Yasunari Shigeta, Haruyoshi Maeda. Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido. Journal of Earth Science, 2012, 23(1). doi: 10.1007/s12583-012-0230-0

Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido

doi: 10.1007/s12583-012-0230-0
  • Received Date: 2017-03-15
  • Rev Recd Date: 2017-03-15
  • Publish Date: 2017-03-15
  • The purpose of this study was to estimate the Coniacian latitudinal thermal gradient in the Northern Hemisphere. Both hemipelagic (ammonoids) and benthic (brachiopods and bivalves) ??18O and ??13С records were used. They originated from Coniacian shallow-water sequences across a wide range of paleolatitudes, from the Koryak upland (northern Kamchatka, Russian Far East) in the north, to Hokkaido (Japan) in the south...
  • 加载中
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(871) PDF downloads(20) Cited by()

Related
Proportional views

Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido

doi: 10.1007/s12583-012-0230-0

Abstract: The purpose of this study was to estimate the Coniacian latitudinal thermal gradient in the Northern Hemisphere. Both hemipelagic (ammonoids) and benthic (brachiopods and bivalves) ??18O and ??13С records were used. They originated from Coniacian shallow-water sequences across a wide range of paleolatitudes, from the Koryak upland (northern Kamchatka, Russian Far East) in the north, to Hokkaido (Japan) in the south...

Yuri D, Olga P, Alexander M, Tatiana A, Tamara B, Kazushige Tanabe, Yasunari Shigeta, Haruyoshi Maeda. Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido. Journal of Earth Science, 2012, 23(1). doi: 10.1007/s12583-012-0230-0
Citation: Yuri D, Olga P, Alexander M, Tatiana A, Tamara B, Kazushige Tanabe, Yasunari Shigeta, Haruyoshi Maeda. Pole to Equator TemperatureGradient for Coniacian Time, Late Cretaceous: Oxygen and Carbon Isotopic Data on the Koryak Upland and Hokkaido. Journal of Earth Science, 2012, 23(1). doi: 10.1007/s12583-012-0230-0

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return