This item requires a subscription to Geology.
Full Text
To view this item, select one of the options below:
Sign In
Purchase Short-Term Access
- Pay per Article - You may access this article (from the computer you are currently using) for 1 day for US$25.00.
- Regain Access - You can regain access to a recent Pay per Article purchase if your access period has not yet expired.
Use or buy Bloc of Docs What's this?
Sign Up
- Subscribe to the Journal - Subscribe to the print and/or online journal.
This Article
-
doi: 10.1130/G19664.1 Geology October 2003 v. 31 no. 10 p. 909-912
- AbstractFree
- Figures Only
- » Full Text
- Full Text (PDF)
Services
Citing Articles
- ABOUT GSA
- JOIN GSA
- SUBSCRIBER SERVICES
- ABOUT GEOLOGY
- AUTHOR INFORMATION
- SCIENCE EDITORS
- DATA REPOSITORY
- E-MAIL ALERTS
- RSS FEEDS
- BLOC OF DOCS
- HELP
- CONTACT US
Most
-
Read
- Rates of sediment delivery from the Fennoscandian Ice Sheet through an ice age
- Reigniting the Cretaceous-Palaeogene firestorm debate
- Fluvial form in modern continental sedimentary basins: Distributive fluvial systems
- Climate-controlled multidecadal variability in North African dust transport to the Mediterranean
- Biomarker reconstruction of the early Eocene paleotopography and paleoclimate of the northern Sierra Nevada
-
Cited
- Reactive bulk assimilation: A model for crust-mantle mixing in silicic magmas
- Late Cenozoic uplift of southeastern Tibet
- Origin of the Rheic Ocean: Rifting along a Neoproterozoic suture?
- Rapid decompression-driven crystallization recorded by melt inclusions from Mount St. Helens volcano
- Evidence from ophiolites, blueschists, and ultrahigh-pressure metamorphic terranes that the modern episode of subduction tectonics began in Neoproterozoic time
