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You searched for subject:(Pseudotachylyte). Showing records 1 – 8 of 8 total matches.

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University of Kentucky

1. Leib, Susan E. THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY.

Degree: 2013, University of Kentucky

 Crustal faulting has long been known as the source of shallow seismicity, and the seismogenic zone is the depth (3-15 km) within the crust that… (more)

Subjects/Keywords: pseudotachylyte; seismogenic zone; crustal depth; thermobarometry; Norway; Geology

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Leib, S. E. (2013). THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY. (Masters Thesis). University of Kentucky. Retrieved from http://uknowledge.uky.edu/ees_etds/9

Chicago Manual of Style (16th Edition):

Leib, Susan E. “THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY.” 2013. Masters Thesis, University of Kentucky. Accessed October 14, 2019. http://uknowledge.uky.edu/ees_etds/9.

MLA Handbook (7th Edition):

Leib, Susan E. “THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY.” 2013. Web. 14 Oct 2019.

Vancouver:

Leib SE. THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY. [Internet] [Masters thesis]. University of Kentucky; 2013. [cited 2019 Oct 14]. Available from: http://uknowledge.uky.edu/ees_etds/9.

Council of Science Editors:

Leib SE. THERMOBAROMETRY OF METAMORPHOSED PSEUDOTACHYLYTE AND DETERMINATION OF SEISMIC RUPTURE DEPTH DURING DEVONIAN CALEDONIAN EXTENSION, NORTH NORWAY. [Masters Thesis]. University of Kentucky; 2013. Available from: http://uknowledge.uky.edu/ees_etds/9


University of Minnesota

2. Longchamp, Benjamin Maxfield. Pseudotachylyte remanence confirms generation along low-angle normal fault planes.

Degree: MS, Earth Sciences, 2019, University of Minnesota

 Low-angle normal faults (LANFs) have been mapped in metamorphic core complexes (MCCs) throughout western North America, but dip too shallowly for seismic slip according to… (more)

Subjects/Keywords: AARM; low-angle normal fault; paleomagnetism; pseudotachylyte; rock magnetism; South Mountains

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APA (6th Edition):

Longchamp, B. M. (2019). Pseudotachylyte remanence confirms generation along low-angle normal fault planes. (Masters Thesis). University of Minnesota. Retrieved from http://hdl.handle.net/11299/206154

Chicago Manual of Style (16th Edition):

Longchamp, Benjamin Maxfield. “Pseudotachylyte remanence confirms generation along low-angle normal fault planes.” 2019. Masters Thesis, University of Minnesota. Accessed October 14, 2019. http://hdl.handle.net/11299/206154.

MLA Handbook (7th Edition):

Longchamp, Benjamin Maxfield. “Pseudotachylyte remanence confirms generation along low-angle normal fault planes.” 2019. Web. 14 Oct 2019.

Vancouver:

Longchamp BM. Pseudotachylyte remanence confirms generation along low-angle normal fault planes. [Internet] [Masters thesis]. University of Minnesota; 2019. [cited 2019 Oct 14]. Available from: http://hdl.handle.net/11299/206154.

Council of Science Editors:

Longchamp BM. Pseudotachylyte remanence confirms generation along low-angle normal fault planes. [Masters Thesis]. University of Minnesota; 2019. Available from: http://hdl.handle.net/11299/206154


Australian National University

3. Hayward, Kathryn Suzanne. The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation .

Degree: 2015, Australian National University

 An experimental study has been undertaken to explore the strength, mechanical behaviour and microstructural evolution of bare interfaces in quartz sandstone during slip. These experiments… (more)

Subjects/Keywords: Frictional melting; amorphisation; faults; experimental rock deformation; fault mechanics; pseudotachylyte

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APA (6th Edition):

Hayward, K. S. (2015). The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation . (Thesis). Australian National University. Retrieved from http://hdl.handle.net/1885/104492

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16th Edition):

Hayward, Kathryn Suzanne. “The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation .” 2015. Thesis, Australian National University. Accessed October 14, 2019. http://hdl.handle.net/1885/104492.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7th Edition):

Hayward, Kathryn Suzanne. “The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation .” 2015. Web. 14 Oct 2019.

Vancouver:

Hayward KS. The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation . [Internet] [Thesis]. Australian National University; 2015. [cited 2019 Oct 14]. Available from: http://hdl.handle.net/1885/104492.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Hayward KS. The strength and mechanical behaviour of quartz slip interfaces: an experimental investigation . [Thesis]. Australian National University; 2015. Available from: http://hdl.handle.net/1885/104492

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation


Kyoto University / 京都大学

4. Ueda, Tadamasa. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究.

Degree: 博士(理学), 2016, Kyoto University / 京都大学

新制・課程博士

甲第19394号

理博第4125号

Subjects/Keywords: pseudotachylyte; brittle-ductile transition; peridotite; ultramylonite

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Ueda, T. (2016). Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究. (Thesis). Kyoto University / 京都大学. Retrieved from http://hdl.handle.net/2433/204571 ; http://dx.doi.org/10.14989/doctor.k19394

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16th Edition):

Ueda, Tadamasa. “Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究.” 2016. Thesis, Kyoto University / 京都大学. Accessed October 14, 2019. http://hdl.handle.net/2433/204571 ; http://dx.doi.org/10.14989/doctor.k19394.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7th Edition):

Ueda, Tadamasa. “Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究.” 2016. Web. 14 Oct 2019.

Vancouver:

Ueda T. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究. [Internet] [Thesis]. Kyoto University / 京都大学; 2016. [cited 2019 Oct 14]. Available from: http://hdl.handle.net/2433/204571 ; http://dx.doi.org/10.14989/doctor.k19394.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Ueda T. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy : 脆性―延性遷移領域における地震性の変形構造:イタリア、バルムチャかんらん岩体に産する超マフィック組成シュードタキライトと随伴する変形岩の研究. [Thesis]. Kyoto University / 京都大学; 2016. Available from: http://hdl.handle.net/2433/204571 ; http://dx.doi.org/10.14989/doctor.k19394

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation


Kyoto University

5. Ueda, Tadamasa. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy .

Degree: 2016, Kyoto University

Subjects/Keywords: pseudotachylyte; brittle-ductile transition; peridotite; ultramylonite

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APA (6th Edition):

Ueda, T. (2016). Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy . (Thesis). Kyoto University. Retrieved from http://hdl.handle.net/2433/204571

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16th Edition):

Ueda, Tadamasa. “Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy .” 2016. Thesis, Kyoto University. Accessed October 14, 2019. http://hdl.handle.net/2433/204571.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7th Edition):

Ueda, Tadamasa. “Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy .” 2016. Web. 14 Oct 2019.

Vancouver:

Ueda T. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy . [Internet] [Thesis]. Kyoto University; 2016. [cited 2019 Oct 14]. Available from: http://hdl.handle.net/2433/204571.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Ueda T. Seismogenic deformation structures in the brittle-ductile transition regime: a case study of ultramafic pseudotachylytes and related deformed rocks in the Balmuccia peridotite body, Italy . [Thesis]. Kyoto University; 2016. Available from: http://hdl.handle.net/2433/204571

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

6. Ferrand, Thomas. Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes.

Degree: Docteur es, Sciences de la Terre et de l'environnement, 2017, Paris Sciences et Lettres

Les séismes intermédiaires (30-300 km) ont été largement documentés dans les plaques océaniques en subduction mais leur mécanisme physique reste énigmatique. Des séismes se produisent… (more)

Subjects/Keywords: Séismes; Manteau; Antigorite; Serpentine; Déshydratation; Pseudotachylite; Earthquakes; Mantle; Antigorite; Serpentine; Dehydration; Pseudotachylyte; 551.1

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Ferrand, T. (2017). Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes. (Doctoral Dissertation). Paris Sciences et Lettres. Retrieved from http://www.theses.fr/2017PSLEE011

Chicago Manual of Style (16th Edition):

Ferrand, Thomas. “Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes.” 2017. Doctoral Dissertation, Paris Sciences et Lettres. Accessed October 14, 2019. http://www.theses.fr/2017PSLEE011.

MLA Handbook (7th Edition):

Ferrand, Thomas. “Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes.” 2017. Web. 14 Oct 2019.

Vancouver:

Ferrand T. Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes. [Internet] [Doctoral dissertation]. Paris Sciences et Lettres; 2017. [cited 2019 Oct 14]. Available from: http://www.theses.fr/2017PSLEE011.

Council of Science Editors:

Ferrand T. Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles : Experimental reproduction of mantle earthquakes analogues by antigorite dehydration & Comparison with natural pseudotachylytes. [Doctoral Dissertation]. Paris Sciences et Lettres; 2017. Available from: http://www.theses.fr/2017PSLEE011


University of Colorado

7. Orlandini, Omero Felipe. The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust.

Degree: PhD, 2019, University of Colorado

  Preserved lower-crustal terranes provide a view into deep earth processes unparalleled in spatial and temporal resolution. We use this rich data set of field… (more)

Subjects/Keywords: electron beam; machine learning; microstructure; petrology; pseudotachylyte; shear zone; Geology; Geotechnical Engineering; Materials Science and Engineering

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APA (6th Edition):

Orlandini, O. F. (2019). The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust. (Doctoral Dissertation). University of Colorado. Retrieved from https://scholar.colorado.edu/geol_gradetds/156

Chicago Manual of Style (16th Edition):

Orlandini, Omero Felipe. “The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust.” 2019. Doctoral Dissertation, University of Colorado. Accessed October 14, 2019. https://scholar.colorado.edu/geol_gradetds/156.

MLA Handbook (7th Edition):

Orlandini, Omero Felipe. “The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust.” 2019. Web. 14 Oct 2019.

Vancouver:

Orlandini OF. The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust. [Internet] [Doctoral dissertation]. University of Colorado; 2019. [cited 2019 Oct 14]. Available from: https://scholar.colorado.edu/geol_gradetds/156.

Council of Science Editors:

Orlandini OF. The Cora Lake Shear Zone: a Natural Laboratory in the Continental Lower Crust. [Doctoral Dissertation]. University of Colorado; 2019. Available from: https://scholar.colorado.edu/geol_gradetds/156


University of Otago

8. Alder, Simon Francis. Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion .

Degree: University of Otago

 Large normal faults are often reactivated as high-angle reverse faults during compressional basin inversion. Although a common situation worldwide, basin inversion is poorly understood from… (more)

Subjects/Keywords: Basin inversion; Moonlight Fault Zone; fault weakening; Pseudotachylyte; Foliated cataclasite; fault reactivation; fault zone structure

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6th Edition):

Alder, S. F. (n.d.). Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion . (Masters Thesis). University of Otago. Retrieved from http://hdl.handle.net/10523/6380

Note: this citation may be lacking information needed for this citation format:
No year of publication.

Chicago Manual of Style (16th Edition):

Alder, Simon Francis. “Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion .” Masters Thesis, University of Otago. Accessed October 14, 2019. http://hdl.handle.net/10523/6380.

Note: this citation may be lacking information needed for this citation format:
No year of publication.

MLA Handbook (7th Edition):

Alder, Simon Francis. “Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion .” Web. 14 Oct 2019.

Note: this citation may be lacking information needed for this citation format:
No year of publication.

Vancouver:

Alder SF. Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion . [Internet] [Masters thesis]. University of Otago; [cited 2019 Oct 14]. Available from: http://hdl.handle.net/10523/6380.

Note: this citation may be lacking information needed for this citation format:
No year of publication.

Council of Science Editors:

Alder SF. Structure and fault rock sequences of the Moonlight Fault Zone, West Otago: constraints on fault reactivation during basin inversion . [Masters Thesis]. University of Otago; Available from: http://hdl.handle.net/10523/6380

Note: this citation may be lacking information needed for this citation format:
No year of publication.

.