981 resultados para 12926-001

Calcium carbonate content of sediment core K708-001

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Physical properties and color of sediment core SO213-001-2

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(Table 38) Chemical composition of grain size fraction <0.001 mm extracted from tholeiitic and alkaline basalt series of the Emperor Mount Chain, DSDP Leg 55

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(Table 43) Chemical composition of grain size fraction <0.001 mm extracted from alkaline basalts of the Meiji Seamount, DSDP Hole 19-192A

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Relative contents of clay minerals in <0.001 mm grain size fraction from recent bottom sediments of the Vistula vermiculite and Neman provinces in the Gdansk Basin, Baltic Sea

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Relative contents of clay minerals in <0.001 mm grain size fraction from recent bottom sediments of the Vistula vermiculite and Neman provinces in the Gdansk Basin, Baltic Sea

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(Table 3) Clay mineral composition of <0.001 mm grain size fraction from red clays of the North Pacific

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Clay mineral composition of <0.001 mm grain size fraction of sedimentary rocks from Hole VNIIO-1984-80 drilled in the Barents Sea

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(Table 1a) Chemical composition of <0.001 mm grain size fraction from bottom sediments of the Philippine Sea

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Clay mineral composition of <0.001 mm grain size fraction of sediments from Hole VNIIO-1990-19 drilled in the Kanin Peninsula

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Clay mineral composition of <0.001 mm grain size fraction of sediments from Hole VNIIO-1990-04 drilled in the Kanin Peninsula

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Clay mineral composition of <0.001 mm grain size fraction of sediments from Hole AMIGE-1993-210 drilled in the Barents Sea

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Clay mineral composition of <0.001 mm grain size fraction of sediments from Hole AMIGE-1993-202 drilled in the Barents Sea

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(Table T40) Chemical composition of grain size fraction <0.001 mm sampled from basalts of alkaline and tholeiitic series, Emperor Seamount chain, Leg 55: Hole 430A (Ojin seamount), Hole 432A (Nintoku seamount), and Hole 433C (Suiko seamount)

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Clay mineral composition of <0.001 mm grain size fraction of sedimentary rocks from Hole Northern-1 drilled in the Alexandra Island, Franz Josef Land Archipelago

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