Magnetic Classification of Stony Meteorites (IV)

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)...

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Bibliographic Details
Main Author: Takesi Nagata
Format: Report
Language:English
Published: National Institute of Polar Research 1979
Subjects:
Memoirs of National Institute of Polar Research
Polar Research
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1061
http://id.nii.ac.jp/1291/00001061/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1061&item_no=1&attribute_id=18&file_no=1
Description
Summary: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.

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