Data/hora: 01/06/2024 12:17:14

Provedor de dados: 	20	
País: 	Belgium	
Título: 	Development of Sedimentary Environment in the Northeastern South China Sea Since the Last Glacial Stage.	
Autores: 	Huangh, Yuanhui; Lan, Dongzhao.	
Data: 	2015-01-21	
Ano: 	2007	
Palavras-chave: 	Grain size; Diatoms; Sedimentary environments.	
Resumo: 	Core D（21°23′02″N，116°47′13″E, water depth 405 m）was sampled from the upper slope from the northeastern South China Sea (SCS) and applied to analyze the sedimentary environmental change in this sea area since the last glacial stage. The results of grain size analysis, diatom analysis and detrital mineral analysis were well matched. We divided the core D into two layers. The surface sand layer (0 - 2 cm) consisted of residual sediments, which might be originally the sediment in the late Pleistocene and later suffered from being transformed in the post glacial transgression. The lower layer (2 - 130 cm) was quite different from the surface one, which might mainly result from a neritic sedimentary environment in the last glacial stage. Two sedimentary cycles could be detected in the core D: regression during Marine isotope stage (MIS) 4 to transgression during MIS 3 and regression during MIS 2 to transgression during the post glacial.	
Tipo: 	Journal Contribution	
Idioma: 	Inglês	
Identificador: 	Marine Science Bulletin, 9 (1),  46-54

1000-9620

http://hdl.handle.net/1834/5836	
Fonte: 	http://creativecommons.org/licenses/by-nc/3.0/