_version_ 1867167662469021696
author Kurnosov, Victor B
author_facet Kurnosov, Victor B
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_730147
institution PANGAEA
language en
publishDate 1982
publisher PANGAEA
record_format pangaea
spellingShingle Mineral and chemical compositions of clay sediments from the Pacific Ocean, DSDP data
Kurnosov, Victor B
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; North Pacific/Bering Strait/RIDGE; North Pacific/Gulf of California/CONT RISE; North Pacific/Gulf of California/DIAPIR; North Pacific/Gulf of California/SEDIMENT POND; North Pacific/GUYOT; North Pacific/Japan Sea/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/TRENCH
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.
title Mineral and chemical compositions of clay sediments from the Pacific Ocean, DSDP data
topic 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; North Pacific/Bering Strait/RIDGE; North Pacific/Gulf of California/CONT RISE; North Pacific/Gulf of California/DIAPIR; North Pacific/Gulf of California/SEDIMENT POND; North Pacific/GUYOT; North Pacific/Japan Sea/CONT RISE; North Pacific/MOUND; North Pacific/RIDGE; North Pacific/TRENCH
url https://doi.org/10.1594/PANGAEA.730147