The preliminary results of a comprehensive study of clay minerals (<2 µm) are presented for the upper 2 m.y. of sediments from Ocean Drilling Program Leg 184 Site 1146 from the northern margin of the South China Sea, close to the Pearl River mouth. More than 500 samples were analyzed, and four main mineral species are present: smectite, illite, chlorite, and kaolinite. On a general basis, illite + chlorite and smectite display anti-correlated behavior in relation to changes in the proportion of primary to secondary minerals in the sediment. Low-frequency and high-frequency changes are observed in the smectite/(illite + chlorite) ratio
Green clay layers are reported from the Pliocene-Holocene intervals in five of the six sites drilled...
This data report documents the acquisition of two new sets of normalization factors for semiquantita...
This paper presents a synthesis of data from X-ray diffraction analyses of clay minerals and X-ray f...
This report describes the results of semiquantitative analysis of clay mineral composition by X-ray ...
International audienceClay mineralogy of surface samples throughout the northeastern South China Sea...
A coupled approach based on clay mineral assemblages and isotopic data (Sr and Nd) of sediment from ...
Three sites were cored on the landward slope of the Nankai margin of southwest Japan during Leg 190 ...
CLAr mineral compositions in specimens of Recent marine sediments in the neighbour-hood of Japan and...
X-ray diffraction studies on the <2-µm fraction of clay samples from cores collected on DSDP Leg ...
International audienceHigh-resolution clay mineralogical analysis of Core MD05-2904 in the northern ...
Sediments recovered from Site 765 can be divided into seven mineral associations, based on differenc...
Samples from Cenozoic and Mesozoic sediments drilled during ODP Leg 103 were analyzed for clay miner...
This report describes the results of semiquantitative analysis of clay mineral composition by X-ray ...
Altogether 513 samples from sediments of Cretaceous to Pleistocene age from DSDP Legs 56 and 57 were...
The clay mineralogy of Lower Cretaceous deep-sea fan sediment in the western North Atlantic is domin...
Green clay layers are reported from the Pliocene-Holocene intervals in five of the six sites drilled...
This data report documents the acquisition of two new sets of normalization factors for semiquantita...
This paper presents a synthesis of data from X-ray diffraction analyses of clay minerals and X-ray f...
This report describes the results of semiquantitative analysis of clay mineral composition by X-ray ...
International audienceClay mineralogy of surface samples throughout the northeastern South China Sea...
A coupled approach based on clay mineral assemblages and isotopic data (Sr and Nd) of sediment from ...
Three sites were cored on the landward slope of the Nankai margin of southwest Japan during Leg 190 ...
CLAr mineral compositions in specimens of Recent marine sediments in the neighbour-hood of Japan and...
X-ray diffraction studies on the <2-µm fraction of clay samples from cores collected on DSDP Leg ...
International audienceHigh-resolution clay mineralogical analysis of Core MD05-2904 in the northern ...
Sediments recovered from Site 765 can be divided into seven mineral associations, based on differenc...
Samples from Cenozoic and Mesozoic sediments drilled during ODP Leg 103 were analyzed for clay miner...
This report describes the results of semiquantitative analysis of clay mineral composition by X-ray ...
Altogether 513 samples from sediments of Cretaceous to Pleistocene age from DSDP Legs 56 and 57 were...
The clay mineralogy of Lower Cretaceous deep-sea fan sediment in the western North Atlantic is domin...
Green clay layers are reported from the Pliocene-Holocene intervals in five of the six sites drilled...
This data report documents the acquisition of two new sets of normalization factors for semiquantita...
This paper presents a synthesis of data from X-ray diffraction analyses of clay minerals and X-ray f...