Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; December 1999; v. 84; no. 11-12; p. 1711-1726
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Johnson, S. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Porphyroblast microstructures; a review of current and future trends

S. E. Johnson

Macquarie University, Department of Earth and Planetary Sciences, Sydney, N.S.W., Australia

Many recent papers show how porphyroblast microstructures play an important role in a wide range of structural and metamorphic studies. This paper reviews ten current applications of these microstructures: (1) porphyroblast growth-timing criteria; (2) tracking progressive foliation development relative to changing metamorphic conditions; (3) timing of pluton emplacement relative to deformation and metamorphism; (4) finite longitudinal strain determinations; (5) kinematics and porphyroblast rotation; (6) use of linear fabrics preserved in porphyroblasts; (7) porphyroblasts and folding mechanisms; (8) inclusion-trail orientations and orogenic processes; (9) inferring shear-strain rates from porphyroblast growth rates; and (10) in-situ age determinations. Although there is still no concensus on the interpretation of some porphyroblast microstructures, a bright future lies ahead as traditional and newly developed techniques of microstructural analysis are combined with modern chemical and microprobe techniques to provide an increased understanding of the relationships between deformation and metamorphism in a wide range of metamorphic settings.

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
GeologyHome page
S. E. Johnson
Porphyroblast rotation and strain localization: Debate settled!
Geology, July 1, 2009; 37(7): 663 - 666.
[Abstract] [Full Text] [PDF]


Home page
GeosphereHome page
P. A. Camilleri
Growth, behavior, and textural sector zoning of biotite porphyroblasts during regional metamorphism and the implications for interpretation of inclusion trails: Insights from the Pequop Mountains and Wood Hills, Nevada, USA
Geosphere, June 1, 2009; 5(3): 215 - 251.
[Abstract] [Full Text] [PDF]


Home page
Eur J MineralHome page
S. Chakraborty, S. Dasgupta, and S. Neogi
Nucleation kinetics controlled by chemical overstepping and its tectonic implications: an example from the Sikkim Himalaya
European Journal of Mineralogy, December 1, 2007; 19(6): 791 - 803.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
C. R. Huddlestone-Holmes and R. A. Ketcham
Getting the inside story: using computed X-ray tomography to study inclusion trails in garnet porphyroblasts
American Mineralogist, November 1, 2005; 90(11-12): ea1 - ea17.
[Abstract] [Full Text] [PDF]


Home page
Can MineralHome page
G. S. Solar and M. Brown
THE CLASSIC HIGH-T - LOW-P METAMORPHISM OF WEST-CENTRAL MAINE: IS IT POST-TECTONIC OR SYNTECTONIC? EVIDENCE FROM PORPHYROBLAST - MATRIX RELATIONS: REPLY
Can Mineral, August 1, 2000; 38(4): 1007 - 1026.
[Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America