Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure
This paper describes riesite, a new high-pressure polymorph of TiO<sub>2</sub> from the Ries impact structure, Germany. Riesite occurs in shock-induced melt veins within xenoliths of bedrock in suevite. It is structurally closely related to srilankite from which it differs by having two...
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Online Access: | https://www.mdpi.com/2075-163X/10/1/78 |
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doaj-dde0991bbfb644088a563977482e6d0e2020-11-25T02:16:09ZengMDPI AGMinerals2075-163X2020-01-011017810.3390/min10010078min10010078Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact StructureOliver Tschauner0Chi Ma1Antonio Lanzirotti2Matthew G. Newville3Department of Geoscience, University of Nevada Las Vegas, Las Vegas, NV 89154, USADivision of Geology and Planetary Sciences, California Institute of Technology, CA 92235, USAGeoSoilEnviroCARS, University of Chicago at the Advanced Photon Source, Argonne National Laboratory, Argonne, IL 60367, USAGeoSoilEnviroCARS, University of Chicago at the Advanced Photon Source, Argonne National Laboratory, Argonne, IL 60367, USAThis paper describes riesite, a new high-pressure polymorph of TiO<sub>2</sub> from the Ries impact structure, Germany. Riesite occurs in shock-induced melt veins within xenoliths of bedrock in suevite. It is structurally closely related to srilankite from which it differs by having two distinct cation sites rather than one and through its monoclinic symmetry. It is indicative that riesite forms only upon release from the shock state upon back transformation from akaogiite.https://www.mdpi.com/2075-163X/10/1/78high-pressure mineralhigh pressuremineral physicsimpacts |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Oliver Tschauner Chi Ma Antonio Lanzirotti Matthew G. Newville |
spellingShingle |
Oliver Tschauner Chi Ma Antonio Lanzirotti Matthew G. Newville Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure Minerals high-pressure mineral high pressure mineral physics impacts |
author_facet |
Oliver Tschauner Chi Ma Antonio Lanzirotti Matthew G. Newville |
author_sort |
Oliver Tschauner |
title |
Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure |
title_short |
Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure |
title_full |
Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure |
title_fullStr |
Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure |
title_full_unstemmed |
Riesite, a New High Pressure Polymorph of TiO<sub>2</sub> from the Ries Impact Structure |
title_sort |
riesite, a new high pressure polymorph of tio<sub>2</sub> from the ries impact structure |
publisher |
MDPI AG |
series |
Minerals |
issn |
2075-163X |
publishDate |
2020-01-01 |
description |
This paper describes riesite, a new high-pressure polymorph of TiO<sub>2</sub> from the Ries impact structure, Germany. Riesite occurs in shock-induced melt veins within xenoliths of bedrock in suevite. It is structurally closely related to srilankite from which it differs by having two distinct cation sites rather than one and through its monoclinic symmetry. It is indicative that riesite forms only upon release from the shock state upon back transformation from akaogiite. |
topic |
high-pressure mineral high pressure mineral physics impacts |
url |
https://www.mdpi.com/2075-163X/10/1/78 |
work_keys_str_mv |
AT olivertschauner riesiteanewhighpressurepolymorphoftiosub2subfromtheriesimpactstructure AT chima riesiteanewhighpressurepolymorphoftiosub2subfromtheriesimpactstructure AT antoniolanzirotti riesiteanewhighpressurepolymorphoftiosub2subfromtheriesimpactstructure AT matthewgnewville riesiteanewhighpressurepolymorphoftiosub2subfromtheriesimpactstructure |
_version_ |
1724892374138617856 |