27 The Enigmatic Late Cretaceous-Paleogene Tectonic Evolution of the Southwestern USA
Wednesday, 13 May 2020
1:30 PM - 5:30 PM
San Rafael
DYNAMICS OF THE POST-SUBDUCTION THERMAL ANOMALY OF THE NACIMIENTO BLOCK REVEALED BY RSCM AND (U-TH/HE) THERMOCHRONOLOGY
Paper number: 27-9
Program: Theme Sessions
Time: 4:05 PM – 4:25 PM
Authors
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Christine WardKansas State University, Manhattan, KS
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Abdeltif LahfidOrléans
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Nathan NiemiUniversity of Michigan, Ann Arbor, MI
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Joel SpencerKansas State University, Manhattan, KS
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Pamela KemptonKansas State University, Manhattan, KS
Abstract
In this contribution we combine regional structural analysis to Raman Spectroscopy on Carbonaceous Material (RSCM) thermometer on samples from the Nacimiento block and present a new peak-temperature distribution map. Our results show an important thermal anomaly (up to 340˚C) in the vicinity of Cape San Martin/Los Burros. Within the thermal anomaly the regional structures are oriented E-W, which significantly contrasts with the regional fabrics generally oriented N315˚-N350˚. This drastic orientation change suggests a counterclockwise rotation of about 50˚- 75˚ compared to the regional fabrics. We infer that the observed rotation of the regional fabrics highlights the presence of a transpressional uplift developed between the SGHF and the Nacimiento Fault during dextral movement, that would explain the exposure more deeply buried and consequently warmer rocks along this apparent thermal anomaly. In order to document the uplift dynamic of this area, we also present new (U-Th)/He dataset on both apatite and zircon from samples collected across the thermal anomaly.
Geological Society of America Abstracts with Programs. Vol. 52, No. 4
doi: 10.1130/abs/2020CD-347351
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