Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change-Reference-Cited by-同舟云学术

Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change

Published:2001-03 Issue:6 Volume:65 Page:901-913
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Ding Z.L.,Sun J.M.,Yang S.L.,Liu T.S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference46 articles.

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4. Variation of Rb/Sr ratios in the loess-paleosol sequences of central China during the last 130,000 years and their implications for monsoon paleoclimatology;Chen;Quat. Res.,1999

5. A coupled environmental system formed at about 2.5 Ma over eastern Asia;Ding;Palaeogeog. Palaeoclim. Palaeoecol.,1992

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