The intensity of saturation magnetization (I_s) and a ratio of the saturation magnetization of α-phase FeNi component to I_s, I_s (α)/I_s, of 1 E-chondrite, 8 H-chondrites, 10 L-chondrites, 3 LL-chondrites, 8 C-chondrites, 6 diogenites, 1 howardite and 3 eucrites are plotted on an I_s versus I_s (α)/I_s diagram. On this diagram, E-, H-, L-, LL- and C-chondrites and achondrites are well separately grouped to be magnetically identified
The saturation magnetization, saturation remanent magnetization, the coercive, and remanent coercive...
The isothermal remanent magnetization (IRM), J_R(H_+H_0), the shock remanent magnetization (SRM), J_...
Three chondrites, Yamato-74160 (LL7), ALH-77260 (L3) and St. Severin (LL6), contain considerable amo...
A database of magnetic susceptibility measurements of stony achondrites (acapulcoitelodranite clan, ...
A magnetic classification of stony meteorites on the basis of their saturation magnetization (I_s) a...
The Prior rule in regard to a relation between Fe°+Ni°and Fe°/Ni°and the Urey-Craig-Mason law in reg...
International audienceA database of magnetic susceptibility (chi) measurements on different non-ordi...
We present a database of magnetic susceptibility measurements on 971 ordinary chondrites. It demonst...
Sixteen iron meteorites are magnetically classified into three major classes; hexahedrite plus Ni-po...
Four parameters of low-field magnetic susceptibility (bulk value, frequency dependence, degree of an...
The magnetic classification of meteorites, based on the measurement of magnetic susceptibility, has ...
The low field magnetic susceptibility, natural remanent magnetization (NRM) and bulk density were me...
13 Yamato stone meteorites have been magnetically examined. They are one enstatite chondrite (E), 6 ...
The paleointensity for a howardite, an ulerite and three diogenites has been determined. By referrin...
The piezo-remanent magnetization (PRM) of Mt. Baldr b (H5-6) and ALH-769 (L6) chondrites and Yamato-...
The saturation magnetization, saturation remanent magnetization, the coercive, and remanent coercive...
The isothermal remanent magnetization (IRM), J_R(H_+H_0), the shock remanent magnetization (SRM), J_...
Three chondrites, Yamato-74160 (LL7), ALH-77260 (L3) and St. Severin (LL6), contain considerable amo...
A database of magnetic susceptibility measurements of stony achondrites (acapulcoitelodranite clan, ...
A magnetic classification of stony meteorites on the basis of their saturation magnetization (I_s) a...
The Prior rule in regard to a relation between Fe°+Ni°and Fe°/Ni°and the Urey-Craig-Mason law in reg...
International audienceA database of magnetic susceptibility (chi) measurements on different non-ordi...
We present a database of magnetic susceptibility measurements on 971 ordinary chondrites. It demonst...
Sixteen iron meteorites are magnetically classified into three major classes; hexahedrite plus Ni-po...
Four parameters of low-field magnetic susceptibility (bulk value, frequency dependence, degree of an...
The magnetic classification of meteorites, based on the measurement of magnetic susceptibility, has ...
The low field magnetic susceptibility, natural remanent magnetization (NRM) and bulk density were me...
13 Yamato stone meteorites have been magnetically examined. They are one enstatite chondrite (E), 6 ...
The paleointensity for a howardite, an ulerite and three diogenites has been determined. By referrin...
The piezo-remanent magnetization (PRM) of Mt. Baldr b (H5-6) and ALH-769 (L6) chondrites and Yamato-...
The saturation magnetization, saturation remanent magnetization, the coercive, and remanent coercive...
The isothermal remanent magnetization (IRM), J_R(H_+H_0), the shock remanent magnetization (SRM), J_...
Three chondrites, Yamato-74160 (LL7), ALH-77260 (L3) and St. Severin (LL6), contain considerable amo...