Kip Hodges
0000-0003-2805-8899
Arizona State University
232 papers found
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Metamorphism, melting, and extension: Age constraints from the High Himalayan Slab of southeast Zanskar and northwest Lahaul
The effects of accretion, erosion and radiogenic heat on the metamorphic evolution of collisional orogens
Neogene cooling and exhumation of upper-amphibolite-facies `whiteschists' in the southwest Pamir Mountains, Tajikistan
Evidence for rapid displacement on Himalayan normal faults and the importance of tectonic denudation in the evolution of mountain ranges – Reply
Short-lived continental magmatic arc at Connemara, western Irish Caledonides. Implications for the age of the Grampian Orogeny
Evolution métamorphique du dôme de Kangmar (Sud-Est-Xizang, Tibet): Implications pour les zones internes himalayennes
Contrasting Oligocene and Miocene thermal histories from the hanging wall and footwall of the South Tibetan detachment in the central Himalaya from40Ar/39Ar thermochronology, Marsyandi Valley, central Nepal
The thermodynamics of Himalayan orogenesis
The thermal structure of collisional orogens as a response to accretion, erosion, and radiogenic heating
Contrasting Oligocene and Miocene thermal histories from the hanging wall and footwall of the South Tibetan detachment in the central Himalaya from 40Ar/39Ar thermochronology, Marsyandi Valley, central Nepal
Metamorphic evolution of the Kangmar dome (Se-Xizang, Tibet): implications for the internal Himalayan zones
40Ar/39Ar geochronology using the laser microprobe
Evidence for rapid displacement on Himalayan normal faults and the importance of tectonic denudation in the evolution of mountain ranges
Petrological and geochronological constraints on regional metamorphism along the northern border of the Bitterroot batholith
Shisha Pangma Leucogranite, South Tibetan Himalaya: Field Relations, Geochemistry, Age, Origin, and Emplacement
Tectonic evolution of the central Annapurna Range, Nepalese Himalayas
The Interdependence of Deformational and Thermal Processes in Mountain Belts
Isotopic constraints on the age and provenance of the Lesser and Greater Himalayan sequences, Nepalese Himalaya
Tectonometamorphic evolution of the Himalayan metamorphic core between the Annapurna and Dhaulagiri, central Nepal
thermochronology of isotopically zoned micas: Insights from the southwestern USA proterozoic orogen
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