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Insights Into the Tectonometamorphic...

Jaramillo Hernandez, Valeria Guadalupe,

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Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California // Valeria Guadalupe Jaramillo Hernandez.
Author:	Jaramillo Hernandez, Valeria Guadalupe,
Description:	1 electronic resource (165 pages)
Notes:	Source: Dissertations Abstracts International, Volume: 86-06, Section: A.
Contained By:	Dissertations Abstracts International86-06A.
Subject:	Geology. -
Online resource:	https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=31765056
ISBN:	9798346855194

Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California /
Jaramillo Hernandez, Valeria Guadalupe,

Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California /Valeria Guadalupe Jaramillo Hernandez. - 1 electronic resource (165 pages)

Source: Dissertations Abstracts International, Volume: 86-06, Section: A.

The North American Cordilleran metamorphic core-complex belt provides insight into the tectonometamorphic evolution of North America. Specifically, the Whipple Mountains metamorphic core complex, or the birthplace of the modern concept of low-angle detachment faulting, has been a target of research for decades. Each project presented in this dissertation addresses scientific questions regarding the deformation history of the Whipple Mountains shear zone which build on each other to provide a holistic view of the geologic history. First, new pressure, temperature, and timing (P-T-t) of deformation constraints were determined for shear zone rocks. The high P-T conditions and the structural relations in the rocks allow for different styles of deformation to be present in the brittle-ductile transition zone at 15-20 km depth where the pore-fluid pressure ratios may be calculated. Finally, a new model is proposed to further explain the formation of the Whipple detachment fault which suggests it may have been active since Mesozoic time. The advancement of analytical tools continues to help bridge the gap between what is known and what can be further discovered, and these projects may help further understand the evolution of the metamorphic core complexes in North America.

English

ISBN: 9798346855194Subjects--Topical Terms:

516570
Geology.
Subjects--Index Terms:

Tectonometamorphic evolution

Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California /
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100 1 $a Jaramillo Hernandez, Valeria Guadalupe, $e author. $3 3814520
245 1 0 $a Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California / $c Valeria Guadalupe Jaramillo Hernandez.
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520 $a The North American Cordilleran metamorphic core-complex belt provides insight into the tectonometamorphic evolution of North America. Specifically, the Whipple Mountains metamorphic core complex, or the birthplace of the modern concept of low-angle detachment faulting, has been a target of research for decades. Each project presented in this dissertation addresses scientific questions regarding the deformation history of the Whipple Mountains shear zone which build on each other to provide a holistic view of the geologic history. First, new pressure, temperature, and timing (P-T-t) of deformation constraints were determined for shear zone rocks. The high P-T conditions and the structural relations in the rocks allow for different styles of deformation to be present in the brittle-ductile transition zone at 15-20 km depth where the pore-fluid pressure ratios may be calculated. Finally, a new model is proposed to further explain the formation of the Whipple detachment fault which suggests it may have been active since Mesozoic time. The advancement of analytical tools continues to help bridge the gap between what is known and what can be further discovered, and these projects may help further understand the evolution of the metamorphic core complexes in North America.
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653 $a North America
653 $a Metamorphic core complexes
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