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Whipp David

Professor of Geodynamic Modelling

Beskrivning

I am a geodynamicist with broad interests in how mountain systems evolve in space and time. I combine field and laboratory data, such as low-temperature thermochronology, with 3D thermo-kinematic and thermo-mechanical numerical models to study actively growing mountains.

Nyckelord

Geodynamics, Tectonics, Geomorphology, Himalayas, Numerical Modeling

Affiliering

Helsingfors universitet
Professor of Geodynamic Modelling
Primär
Geosciences and Geography
2021
Primär
Källa: ORCID
Dalhousie University
Adjunct of the Faculty of Graduate Studies
Earth Sciences
2013 - nuvarande
Källa: ORCID
Helsingfors universitet
Associate Professor of Geodynamic Modelling
Geosciences and Geography
2017 - 2020
Källa: ORCID
Helsingfors universitet
Assistant Professor of Geodynamic Modelling
Geosciences and Geography
2013 - 2016
Källa: ORCID
Dalhousie University
Postdoctoral researcher
Oceanography
2009 - 2012
Källa: ORCID
Université de Rennes 1
Postdoctoral researcher
Géosciences
2008 - 2009
Källa: ORCID
University of Michigan
Research Assistant
Geological Sciences
2003 - 2008
Källa: ORCID
ExxonMobil Exploration Company
Geoscientist (intern)
2007
Källa: ORCID

Utbildning (2)

Ph.D.
University of Michigan
B.S.
University of Michigan

Publikationer (20)

2023
Exploring the relationships between low-temperature thermochronometers, temperature-time histories, and geological processes using Tc1D
DOI
10.5194/egusphere-egu23-12472
Records of continent-continent collisions in the Paleoproterozoic: exploring the effects of convergence obliquity and temperature on P-T-t paths
DOI
10.5194/egusphere-egu23-15948
2022
Short communication: Modeling competing effects of cooling rate, grain size, and radiation damage in low-temperature thermochronometers
DOI
10.5194/gchron-4-143-2022

Data (1)

2021
Öppen tillgång

Beviljade finansiering (3)

Finlands Akademi
2023 - 2027
What controls strain partitioning at obliquely convergent ocean-continent margins? 3D dynamics of crustal deformation along the western Andean margin
University of Helsinki Research Funds
2014 - 2017
What controls deformation in a ‘bent’ 3D orogen? The effects of spatially variable rock strength, erosion and mass transport on the tectonics of the Bolivian Andes
Finlands Akademi
2014 - 2018