High-resolution electron microscopy of olivine-magnetite interfaces

Stuart Mckernan; C. Barry Carter

High-resolution electron microscopy of olivine-magnetite interfaces

Stuart Mckernan
, C. Barry Carter

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution

Abstract

In the oxidation of iron-rich olivine (Mg, Fe)2SiO4 at elevated temperatures interfaces between olivine and the magnetite spinel (Fe3O4) are formed. The orientation relation between these structures is such that the planar spacing for the principal low index planes are very closely matched in the two materials. Regions of different contrast is due toe enhanced iron concentration in this region caused by the strain field around the magnetite precipitates.

Original language	English
Title of host publication	Materials Research Society Symposium Proceedings
Pages	553-556
Number of pages	4
Volume	280
State	Published - Dec 1 1993
Externally published	Yes

Cite this

@inproceedings{18067d5488b64c4a8cb0a8ad9ac8f7dd,

title = "High-resolution electron microscopy of olivine-magnetite interfaces",

abstract = "In the oxidation of iron-rich olivine (Mg, Fe)2SiO4 at elevated temperatures interfaces between olivine and the magnetite spinel (Fe3O4) are formed. The orientation relation between these structures is such that the planar spacing for the principal low index planes are very closely matched in the two materials. Regions of different contrast is due toe enhanced iron concentration in this region caused by the strain field around the magnetite precipitates.",

author = "Stuart Mckernan and Carter, \{C. Barry\}",

year = "1993",

month = dec,

day = "1",

language = "English",

isbn = "1558991751",

volume = "280",

pages = "553--556",

booktitle = "Materials Research Society Symposium Proceedings",

}

TY - GEN

T1 - High-resolution electron microscopy of olivine-magnetite interfaces

AU - Mckernan, Stuart

AU - Carter, C. Barry

PY - 1993/12/1

Y1 - 1993/12/1

N2 - In the oxidation of iron-rich olivine (Mg, Fe)2SiO4 at elevated temperatures interfaces between olivine and the magnetite spinel (Fe3O4) are formed. The orientation relation between these structures is such that the planar spacing for the principal low index planes are very closely matched in the two materials. Regions of different contrast is due toe enhanced iron concentration in this region caused by the strain field around the magnetite precipitates.

AB - In the oxidation of iron-rich olivine (Mg, Fe)2SiO4 at elevated temperatures interfaces between olivine and the magnetite spinel (Fe3O4) are formed. The orientation relation between these structures is such that the planar spacing for the principal low index planes are very closely matched in the two materials. Regions of different contrast is due toe enhanced iron concentration in this region caused by the strain field around the magnetite precipitates.

UR - https://www.scopus.com/pages/publications/0027831241

M3 - Conference contribution

SN - 1558991751

VL - 280

SP - 553

EP - 556

BT - Materials Research Society Symposium Proceedings

ER -

High-resolution electron microscopy of olivine-magnetite interfaces

Abstract

Fingerprint

Cite this