We are upgrading the repository! A content freeze is in effect until December 6th, 2024 - no new submissions will be accepted; however, all content already published will remain publicly available. Please reach out to repository@u.library.arizona.edu with your questions, or if you are a UA affiliate who needs to make content available soon. Note that any new user accounts created after September 22, 2024 will need to be recreated by the user in November after our migration is completed.

Apatite and zircon fission-track dates from the northern Plomosa Mountains, La Paz County, west-central Arizona

Thumbnail
Name:
OFR_92_9.pdf
Size:
1.094Mb
Format:
PDF
Download
Author
Foster, D.A.
Spencer, J.E.
Issue Date
1992-10-13
Keywords
Arizona Geological Survey Open File Reports
Plomosa Mountains
La Paz County
Arizona
faults
crustal extension tectonics
fission-tracking
zircon
apatite
Proterozoic

Metadata
Show full item record
Citation
Foster, D.A. and Spencer, J.E., 1992, Apatite and zircon fission-track dates from the northern Plomosa Mountains, La Paz County, west-central Arizona. Arizona Geological Survey Open File Report, OFR-92-09, 11 p.
Description
Fission-track thermochronologic data have the potential to reveal aspects of the timing, rate, and style of crustal extension tectonics. Previous fission-track studies in the footwalls of detachment faults in the Basin and Range Province of western North America have found monotonic decreases in apparent fission-track age in the slip direction of the faults (e.g., Fitzgerald and others, 1991; Foster and others, 1991, in press). This pattern has been interpreted as recording the time at which progressively deeper parts of the footwalls to the detachments have moved through the annealing zone for fission-tracks in apatite. In this study we analyzed fission-tracks in apatite and zircon from samples of Proterozoic crystalline rock from a south to north transect across the northern Plomosa Mountains, Arizona (Figure 1). The transect runs from about 100 meters structurally below the Tertiary unconformity (DF90-226) north to the deepest exposed structural levels in the range (DF90-220) beneath the Tertiary Plomosa detachment fault (Scarborough and Meader, 1981). In addition, one sample (DF90-221) is from a detached block of basement in the hanging wall of the Plomosa fault in the northern-most part of the range. The fission-track data from these samples constrain the low temperature (<250 C) thermal history of the northern Plomosa Mountains and have implications for the timing and rate of displacement on the Plomosa detachment. The data also have implications for nature of extension in this range which occupied a position near the breakaway region for detachments in the Whipple tilt domain (Spencer and Reynolds, 1991). ( 11 pages )
URI
http://hdl.handle.net/10150/629648
Additional Links
https://library.azgs.arizona.edu/
Language
en
Series/Report no.
OFR-92-09
Rights
Arizona Geological Survey. All rights reserved.
Collection Information
Documents in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
North Bounding Coordinate
34.2254
South Bounding Coordinate
33.7883
West Bounding Coordinate
-113.752
East Bounding Coordinate
-113.148
Collections