THE INFLUENCE OF BIOGENIC OPAL ON THE RESULTS OF GRAIN SIZE ANALYSIS OF SURFACE SEDIMENTS IN THE SOUTHERN SOUTH CHINA SEA

ZHANG Jin; LI Anchun; WAN Shiming; HUANG Jie; LU Jian; JIANG Fuqing; LI Tiegang

doi:10.16562/j.cnki.0256-1492.2016.03.004

Marine Geology & Quaternary Geology > 2016 > 36(3): 35-46. > DOI: 10.16562/j.cnki.0256-1492.2016.03.004

ZHANG Jin, LI Anchun, WAN Shiming, HUANG Jie, LU Jian, JIANG Fuqing, LI Tiegang. THE INFLUENCE OF BIOGENIC OPAL ON THE RESULTS OF GRAIN SIZE ANALYSIS OF SURFACE SEDIMENTS IN THE SOUTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(3): 35-46. DOI: 10.16562/j.cnki.0256-1492.2016.03.004

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THE INFLUENCE OF BIOGENIC OPAL ON THE RESULTS OF GRAIN SIZE ANALYSIS OF SURFACE SEDIMENTS IN THE SOUTHERN SOUTH CHINA SEA

1. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071;
2. Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061

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Received Date: October 29, 2015
Revised Date: November 26, 2015

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Abstract

Abstract

Two different pretreatment methods were used to measure grain size of surface sediments collected from the Southern South China Sea, and the influence of the biogenic opal on the grain size results were evaluated. The grain size results show that all the grain size fractions, grain size parameters, and the sediment classification were significantly influenced by the existence of biogenic opal. Based on the volume percentage of siliceous bioclastic, to construct the grain size distribution pattern of the terrestrial sediments on the Nansha Continental Slope, it is necessary to remove biogenic opal from samples in pretreatment. Comparison between the grain size results of two pretreatment methods suggest that the biogenic opal mainly occur in the range of 8 to 90 micron.
- biogenic opal,
- grain size,
- pretreatment methods,
- Southern South China Sea

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References (77)

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THE INFLUENCE OF BIOGENIC OPAL ON THE RESULTS OF GRAIN SIZE ANALYSIS OF SURFACE SEDIMENTS IN THE SOUTHERN SOUTH CHINA SEA