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999 resultados para B-lattice

(Table 74) Parameter b of clay minerals from veins and pore fillings of basalts from Nauru Basin at DSDP Site 61-462

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(Table 71) Parameter b of clay minerals from the main basalt mass of the Nauru Basin, DSDP Site 61-462

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(Table 40) Parameter b for clay minerals replacing olivines in basalts of tholeiitic and alkaline series from the Emperor Seamount Chain, DSDP Leg 55

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(Table 11) Parameter b of clay minerals and polytype of hydromica from sediments at DSDP Site 65-485

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(Table T47) Parameter b of clay minerals replacing olivines in basalts of alkaline and tholeiitic series from Emperor Seamount chain, Leg 55: Holes 433A and 433C (Suiko seamount)

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(Table T53) Parameter b of clay minerals in fine fraction sampled from alkaline basalts of Emperor Seamount chain, Leg 19: Hole 192A (Meiji seamount)

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(Table 35) Parameter b of clay minerals and polytypes of hydromica from sediments of the Aleutian Basin in DSDP Hole 19-190

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(Table 17) Parameter b of smectites from sediments of the Galapagos hydrothermal Mound Field, DSDP Hole 70-506C

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(Table 21) Parameter b of clay minerals and polytypes of hydromica from sediments of the Meiji Guyot at DSDP Site 19-192

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(Table 71) Parameter b of smectites from sediments of the Nauru Basin at DSDP Site 61-462

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(Table T39) Parameter b of clay minerals sampled from basalts of alkaline and tholeiitic series from Emperor Seamount chain, Leg 55: Hole 430A (Ojin seamount), Hole 432A (Nintoku seamount), and Hole 433C (Suiko seamount)

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(Table 45) Parameter b for clay minerals filling interstices in basalts of tholeiitic and alkaline series from the Emperor Seamount Chain, DSDP Leg 55

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(Table 10) Parameter b of smectites from the main mass, veins, and altered zones of basalts drilled in the California Gulf, DSDP Hole 65-485A

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(Table 46) Parameter b of clay minerals and polytypes of hydromica from sediments of the Japan Trench at DSDP Site 56-434

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(Table 26) Parameter b of clay minerals and polytypes of hydromica from sediments of the Bowers Ridge in DSDP Hole 19-188

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