東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Insights Into the Tectonometamorphic...

Jaramillo Hernandez, Valeria Guadalupe,

FindBook

Google Book

Amazon

博客來

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

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Insights Into the Tectonometamorphic Evolution of the Whipple Mountains Ductile Shear Zone, Southeastern California // Valeria Guadalupe Jaramillo Hernandez.
作者:	Jaramillo Hernandez, Valeria Guadalupe,
面頁冊數:	1 electronic resource (165 pages)
附註:	Source: Dissertations Abstracts International, Volume: 86-06, Section: A.
Contained By:	Dissertations Abstracts International86-06A.
標題:	Geology. -
電子資源:	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 /
LDR:02866nmm a22004453i 4500 001 2427584
005 20260911085207.5
006 m o d
007 cr|nu|||||||||
008 260929s2024 miu||||||m |||||||eng d
020 $a 9798346855194
035 $a (MiAaPQD)AAI31765056
035 $a AAI31765056
040 $a MiAaPQD $b eng $c MiAaPQD $e rda
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.
264 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2024
300 $a 1 electronic resource (165 pages)
336 $a text $b txt $2 rdacontent
337 $a computer $b c $2 rdamedia
338 $a online resource $b cr $2 rdacarrier
500 $a Source: Dissertations Abstracts International, Volume: 86-06, Section: A.
500 $a Advisors: Manning, Craig E. Committee members: Day, Mackenzie D.; Harrison, Timothy Mark; Peltzer, Gilles F.
502 $b Ph.D. $c University of California, Los Angeles $d 2024.
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.
546 $a English
590 $a School code: 0031
650 4 $a Geology. $3 516570
650 4 $a American studies. $3 2122720
650 4 $a Petrology. $3 535210
650 4 $a Geochemistry. $3 539092
653 $a Tectonometamorphic evolution
653 $a Whipple Mountains
653 $a Shear zone rocks
653 $a North America
653 $a Metamorphic core complexes
690 $a 0372
690 $a 0323
690 $a 0996
690 $a 0584
710 2 $a University of California, Los Angeles. $b Geology 0402. $e degree granting institution. $3 3814521
720 1 $a Manning, Craig E. $e degree supervisor.
773 0 $t Dissertations Abstracts International $g 86-06A.
790 $a 0031
791 $a Ph.D.
792 $a 2024
856 4 0 $u https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=31765056