Download presentation
Presentation is loading. Please wait.
1
Tilted middle Tertiary ash-flow calderas and subjacent granitic plutons, southern Stillwater Range, Nevada : Cross sections of an Oligocene igneous center By David A. John
2
Introduction Steeply tilted late Oligocene caldera system record a number of unusual features Extremely thick (>4-5.5 km) caldera related deposits Lack of evidence of structural doming Preservation of compositional zoning Cogenetic plutonic rocks are exposed over depth range of~10 km
6
Stillwater Caldera Complex Job Canyon (29-28 Ma) Poco Canyon (25-23 Ma) Eleven Mile Canyon (25-23 Ma) Composite Freeman Creek pluton
10
Unusual features Extreme thickness caldera related deposits (>4-5.5 km)
13
Unusual features continued Preservation of compositional zoning
15
Caldera collapse Miocene extension Basement rocks tilted 40°-90° Subvertical ring-fracture faults (>3-5 km) depth Piston like blocks Lack of evidence of structural doming
19
Conclusions Oligocene caldera complex in the southern Stillwater Range Extremely thick caldera related deposits due to extreme subsidence Cogenetic plutonic rocks over a depth range of ~10 km due to tilting during Miocene extension
Similar presentations
© 2024 SlidePlayer.com Inc.
All rights reserved.