Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; October 2006; v. 91; no. 10; p. 1509-1520; DOI: 10.2138/am.2006.2177
© 2006 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
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 Similar articles in ISI Web of Science
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 ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by MacPherson, G. J.
Right arrow Articles by Phipps, S. P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Tectonic implications of diverse igneous blocks in Franciscan mélange, Northern California and southwestern Oregon

Glenn J. MacPherson1,*, Mario J. Giaramita2 and Stephen Paul Phipps3

1 Department of Mineral Sciences, U.S. National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560, U.S.A.
2 Department of Physics and Geology, California State University at Stanislaus, Turlock, California 95382, U.S.A.
3 Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania 19104-6316, U.S.A.

Correspondence: * E-mail: glenn{at}volcano.si.edu

More than 50% of the igneous blocks from mélanges of the Franciscan subduction complex in northernmost California and from the equivalent Dothan Formation of southwestern Oregon are more silica-rich than basalt, and some contain supra-subduction zone geochemical signatures such as elevated Th/Ta ratios. In contrast, blocks from more southerly parts of the Franciscan mélange belt are more commonly mid-ocean ridge and ocean island/seamount basalts. The data indicate a north-south variation in the block population, due to differences in source terrane, or in the processes that provided the blocks and transported them into the mélange, or both. We suggest that, in the northern Franciscan, a relatively greater fraction of igneous mélange blocks was emplaced by block slumping from the forearc crust into the trench than was the case to the south.

Key Words: Franciscan • igneous blocks • mélange • geochemistry




This article has been cited by other articles:


Home page
Geol Soc Am BullHome page
W.G. Ernst, C. A. Snow, and H. H. Scherer
Contrasting early and late Mesozoic petrotectonic evolution of northern California
GSA Bulletin, January 1, 2008; 120(1-2): 179 - 194.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of America