Mineral and chemical compositions of clay sediments from the Pacific Ocean, DSDP data

• Main Author: Kurnosov, Victor B
• Format: Dataset
• Language: English
• Published: PANGAEA 1982
• Subjects: 19-188; 19-190; 19-191; 19-191A; 19-191B; 19-192; 19-192A; 31-301; 56-434; 56-434B; 56-435; 56-435A; 56-436; 61-462; 61-462A; 65-482A; 65-482B; 65-482C; 65-482D; 65-482F; 65-483; 65-483B; 65-484A; 65-485; 65-485A; 67-494; 67-494A; 67-495; 67-496; 67-499; 67-499B; 70-506C; 70-506D; 70-507D; 70-509B; Archive of Ocean Data; ARCOD; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg19; Leg31; Leg56; Leg61; Leg65; Leg67; Leg70; North Pacific/Bering Strait/BASIN; Bering Strait; Pacific
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.730147; https://doi.org/10.1594/PANGAEA.730147

Mineral and chemical compositions, as well as conditions of formation of clay sediments in major structural elements of the Pacific Ocean floor with different ages are under consideration in the monograph. Depending on evolution of the region two ways of clay sediment formation are identified: terrigenous and authigenic. It is shown that terrigenous clay sediments predominate in marginal parts of the Pacific Ocean. Authigenic mineral formation occurring in the basal part of the sedimentary cover primarily results from removal of material from underlying basalts. This material is released during secondary alteration of the basalts due to their interaction with sea water, as well as with deep solutions.