Chemical composition of clinoptilolite crystals from ODP Hole 108-661A (Table 2), supplement to: Bohrmann, Gerhard; Stein, Ruediger; Faugeres, Jean-Claude (1989): Authigenic zeolites and their relation to silica diagenesis in ODP Site 661sediments (Leg 108, Eastern Equatorial Atlantic). Geologische Rundschau, 78(3), 779-792

Gerhard Bohrmann, Ruediger Stein & Jean-Claude Faugeres
At ODP Site 661 from the continental margin of Northwest Africa, authigenic clinoptilolites were investigated in detail. Based on chemical data, crystal size and shape and their intergrowth with associated mineral phases, two types of clinoptilolite (type A and B) occur representing different diagenetic conditions under which the formation of zeolites took place. Clinoptilolite type A was found in a sediment section comprises numerous hiatuses and stratigraphically condensed sediments and could have been formed during...
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