In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 123, No. 4 ( 2018-04), p. 2522-2538
Abstract:
Fine grained nanometer‐sized magnetite, maghemite, and hematite are the main iron oxides in burnt daub remains from Neolithic houses Paleo‐firing temperatures determined with magnetic susceptibility method are notably high; they range between 680 and 1,140°C Iron oxides' magnetic properties resemble those of particles synthesized by the solution combustion method
Type of Medium:
Online Resource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1002/2017JB015190
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2016813-5
detail.hit.zdb_id:
161666-3
detail.hit.zdb_id:
3094197-0
SSG:
16,13