Temperature and pressure of mylonitization in a Tertiary extensional shear zone, Ruby Mountains-East Humboldt Range, Nevada: tectonic implications

H. A. Hurlow, A. W. Snoke, Kip Hodges

Research output: Contribution to journalArticle

35 Citations (Scopus)

Abstract

In the northern Ruby Mountains-East Humboldt Range metamorphic core complex, a kinematically coupled mylonitic shear zone and brittle-plastic detachment fault compose a low-angle extensional fault system that is mid-Tertiary in age. Geothermobarometry of pelitic schists from the mylonitic shear zone yields a temperature and pressure estimate of 820-900 K (580-620°C) and 310-370 MPa (3.1-3.7 kbar) for mylonite petrogenesis. The shear-zone-detachment-fault system excised 11-12 km of crustal section and accommodated at least 15-17 km of normal-sense dip slip. -Authors

Original languageEnglish (US)
Pages (from-to)82-86
Number of pages5
JournalGeology
Volume19
Issue number1
DOIs
StatePublished - 1991
Externally publishedYes

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mylonitization
ruby
shear zone
detachment fault
tectonics
mountain
dip-slip fault
mylonite
temperature
petrogenesis
schist
plastic

ASJC Scopus subject areas

  • Geology

Cite this

Temperature and pressure of mylonitization in a Tertiary extensional shear zone, Ruby Mountains-East Humboldt Range, Nevada : tectonic implications. / Hurlow, H. A.; Snoke, A. W.; Hodges, Kip.

In: Geology, Vol. 19, No. 1, 1991, p. 82-86.

Research output: Contribution to journalArticle

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