Holk, Gregory J. and Taylor, Bruce E. and Taylor, Hugh P., Jr. (1997) Influx of low D/H meteoric water into the lower plates of metamorphic core complexes, southeastern British Columbia. Abstracts with Programs - Geological Society of America, 29 (6). p. 449. ISSN 0016-7592. https://resolver.caltech.edu/CaltechAUTHORS:20130820-135356479
Full text is not posted in this repository.
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20130820-135356479
Abstract
It is now well established that the upper plates of metamorphic core complexes in British Columbia underwent intense meteoric-hydrothermal alteration at high water-rock ratios (W/R) in the brittle fracturing regime during Eocene extension (Magaritz and Taylor, 1986, Nesbitt and Muehlenbachs, 1989, Beaudoin et al., 1991). Also, quartz-feldspar ^(18)O/^(16)O disequilibrium in the basement Monashee complex and Monashee decollement imbricate thrust zone (MD) indicates that these meteoric-hydrothermal fluids at 1east locally affected the lower plates (Holk and Taylor, 1997).
| Item Type: | Article |
|---|---|
| Additional Information: | © 1997 Geological Society of America. |
| Issue or Number: | 6 |
| Record Number: | CaltechAUTHORS:20130820-135356479 |
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20130820-135356479 |
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. |
| ID Code: | 40742 |
| Collection: | CaltechAUTHORS |
| Deposited By: | Tony Diaz |
| Deposited On: | 23 Aug 2013 22:15 |
| Last Modified: | 03 Oct 2019 05:42 |
Repository Staff Only: item control page
