Evidence for large-scale transport on the Bullard detachment fault, west-central Arizona.

Stephen Reynolds, J. E. Spencer

Research output: Contribution to journalArticle

64 Citations (Scopus)

Abstract

The Bullard detachment fault is a gently to steeply dipping normal fault that flanks the Harcuvar and Harquahala mountains of the Basin and Range province in W-central Arizona. The stratigraphy of upper-plate Miocene conglomerates and the regional distribution of upper- and lower-plate pre-Tertiary units indicate that upper-plate rocks were displaced approx 50km to the NE with respect to the lower plate during middle to late Tertiary time. Normal slip of this magnitude on the regionally NE-dipping Bullard fault indicates that deep-seated Tertiary-Cretaceous(?) mylonitic gneisses and Mesozoic thrust faults of the lower plate were drawn out from beneath Precambrian rocks along the margin of the Transition Zone of central Arizona during middle to late Tertiary crustal extension. The Transition Zone was, therefore, affected by deep-seated tectonism in both Mesozoic and Tertiary time.-Authors

Original languageEnglish (US)
Pages (from-to)353-356
Number of pages4
JournalGeology
Volume13
Issue number5
DOIs
StatePublished - 1985
Externally publishedYes

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detachment fault
transition zone
thrust fault
rock
normal fault
conglomerate
Precambrian
stratigraphy
Miocene
Cretaceous
mountain
basin

ASJC Scopus subject areas

  • Geology

Cite this

Evidence for large-scale transport on the Bullard detachment fault, west-central Arizona. / Reynolds, Stephen; Spencer, J. E.

In: Geology, Vol. 13, No. 5, 1985, p. 353-356.

Research output: Contribution to journalArticle

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