_version_ 1867168545882767360
author Zhang, Yang
Wang, Wanzhang
author_facet Zhang, Yang
Wang, Wanzhang
collection Datos científicos de ciencias marinas y ambientales
contents End-member unmixing using the algorithm of Heslop and Dillon (2007) (doi:10.1111/j.1365-246X.2007.03432.x) was performed on 65 normalized IRM acquisition curves to quantify relative concentration changes of major magnetic mineral fractions. Four separate endmember components EM 1–4 were indicated. EM1 and EM2 represent ferrimagnetic low-coercivity components, which are saturated at 100 and 300 mT, respectively. EM3 and EM4 are still far from saturation at 500 mT and should primarily include the antiferromagnetic high-coercivity minerals hematite and goethite.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_991428
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Endmember analysis of IRM acquisition curves of 65 sediment samples of IODP Site 378-U1553, southern Campbell Plateau
Zhang, Yang
Wang, Wanzhang
378-U1553A; 378-U1553B; 378-U1553E; Calculated average/mean values; DC Pulse Magnetization Step; Depth, composite revised; Depth correlation/correction; Diagenesis; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; End member 1; End member 2; End member 3; End member 4; End-member analysis; End member description; Event label; Exp378; International Ocean Drilling Programme; IODP3; IODP 378; IRM, Intensity, per unit volume; Joides Resolution; Magnetization, normalized; Magnetometer, cryogenic, pass-through, 2G Enterprises 755 R; Magnetostratigraphy; rock magnetism; Sample code/label; South Pacific; South Pacific Ocean
End-member unmixing using the algorithm of Heslop and Dillon (2007) (doi:10.1111/j.1365-246X.2007.03432.x) was performed on 65 normalized IRM acquisition curves to quantify relative concentration changes of major magnetic mineral fractions. Four separate endmember components EM 1–4 were indicated. EM1 and EM2 represent ferrimagnetic low-coercivity components, which are saturated at 100 and 300 mT, respectively. EM3 and EM4 are still far from saturation at 500 mT and should primarily include the antiferromagnetic high-coercivity minerals hematite and goethite.
title Endmember analysis of IRM acquisition curves of 65 sediment samples of IODP Site 378-U1553, southern Campbell Plateau
topic 378-U1553A; 378-U1553B; 378-U1553E; Calculated average/mean values; DC Pulse Magnetization Step; Depth, composite revised; Depth correlation/correction; Diagenesis; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; End member 1; End member 2; End member 3; End member 4; End-member analysis; End member description; Event label; Exp378; International Ocean Drilling Programme; IODP3; IODP 378; IRM, Intensity, per unit volume; Joides Resolution; Magnetization, normalized; Magnetometer, cryogenic, pass-through, 2G Enterprises 755 R; Magnetostratigraphy; rock magnetism; Sample code/label; South Pacific; South Pacific Ocean
url https://doi.org/10.1594/PANGAEA.991428