Al 3 Si 2 O 7 (OH) 3 , phase Pi (formerly piezotite); crystal structure of a synthetic high-pressure silicate rediscovered

Peter Daniels; Bernd Wunder

Article navigation

Other| December 01, 1996

Al ₃ Si ₂ O ₇ (OH) ₃ , phase Pi (formerly piezotite); crystal structure of a synthetic high-pressure silicate rediscovered

Peter Daniels;

Peter Daniels

Ruhr-Universitaet Bochum, Institut fuer Mineralogie, Bochum, Federal Republic of Germany

Search for other works by this author on:

GSW

Google Scholar

Bernd Wunder

Search for other works by this author on:

GSW

Google Scholar

Author and Article Information

Peter Daniels

Ruhr-Universitaet Bochum, Institut fuer Mineralogie, Bochum, Federal Republic of Germany

Bernd Wunder

Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie

First Online: 02 Mar 2017

Online ISSN: 1617-4011

Print ISSN: 0935-1221

European Journal of Mineralogy (1996) 8 (6): 1283–1292.

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

You could not be signed in. Please check your email address / username and password and try again.

Shibboleth Sign In

OpenAthens Sign In

Institutional Sign In

Al ₃ Si ₂ O ₇ (OH) ₃ , phase Pi (formerly piezotite); crystal structure of a synthetic high-pressure silicate rediscovered

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

Al 3 Si 2 O 7 (OH) 3 , phase Pi (formerly piezotite); crystal structure of a synthetic high-pressure silicate rediscovered

First Page Preview

Email alerts

Citing articles via

About GSW

Resources

Explore

Connect

This Feature Is Available To Subscribers Only

Al ₃ Si ₂ O ₇ (OH) ₃ , phase Pi (formerly piezotite); crystal structure of a synthetic high-pressure silicate rediscovered