ELEMENT GEOCHEMISTRY OF THE SECOND MEMBER OF KONGDIAN FORMATION IN SOUTHERN HUANGHUA DEPRESSION AND ITS IMPLICATIONS

WANG Jianqiang; ZHANG Jianwei; XUE Linfu; SUN Jing

doi:10.3724/SP.J.1140.2015.01061

Marine Geology & Quaternary Geology > 2015 > 35(1): 61-69. > DOI: 10.3724/SP.J.1140.2015.01061

WANG Jianqiang, ZHANG Jianwei, XUE Linfu, SUN Jing. ELEMENT GEOCHEMISTRY OF THE SECOND MEMBER OF KONGDIAN FORMATION IN SOUTHERN HUANGHUA DEPRESSION AND ITS IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 61-69. DOI: 10.3724/SP.J.1140.2015.01061

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ELEMENT GEOCHEMISTRY OF THE SECOND MEMBER OF KONGDIAN FORMATION IN SOUTHERN HUANGHUA DEPRESSION AND ITS IMPLICATIONS

1. Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;

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Received Date: February 09, 2014
Revised Date: March 09, 2014

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Abstract

Abstract

Lithology, trace elements and rare earth elements were studied for the 5 fresh samples of carbonaceous mudstone taken from the 2nd Member of the Kongdian Formation in the southern Huanghua Depression. X fluorescence and ICP-MS are used for determination of element geochemistry and barium strontium method (Sr/Ba), boron gallium method (B/Ga), boron element method (B) and C, O isotope method used for restoration of paleo-salinity. Upon the basis, the paleo-climatic environment and the openness of the basin are discussed. The results show that during the period while the 2nd Member of the Kongdian Formation was deposited, the climate was humid, and rich in rainfall. It was a closed inland lake basin filled with fresh or subsaline water. The La-Th-Sc, Th-Sc-Zr/10 diagrams and the characteristics of rare earth elements show that the study area was tectonically a marginal depression along an active continental margin. The mudstone is low in rare earth elements (∑REE=135.14~190.6), and high in light rare earth elements (LREE/HREE=9.44~10.96), with negative abnormal Eu (δEu=0.54~0.71), suggesting a granite dominated source area with some sedimentary rocks.
- Huanghua Depression,
- the 2nd Member of Kongdian Formation,
- carbonaceous mudstone,
- paleo-climatic environment,
- closeness

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ELEMENT GEOCHEMISTRY OF THE SECOND MEMBER OF KONGDIAN FORMATION IN SOUTHERN HUANGHUA DEPRESSION AND ITS IMPLICATIONS

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