Whipp, David
https://orcid.org/0000-0002-3820-6886 Professor of Geodynamic Modelling, Helsingin yliopisto
Tutkimustoiminnan kuvaus
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.Avainsanat
Geodynamics, Tectonics, Geomorphology, Himalayas, Numerical ModelingAffiliaatiot
Helsingin yliopisto
Yksikkö
Geosciences and Geography
Lähde: ORCID
Nimike
Professor of Geodynamic Modelling 2021 -
Yksikkö
Geosciences and Geography
Lähde: ORCID
Nimike
Associate Professor of Geodynamic Modelling 2017 - 2020
Yksikkö
Geosciences and Geography
Lähde: ORCID
Nimike
Assistant Professor of Geodynamic Modelling 2013 - 2016
Dalhousie University
Yksikkö
Earth Sciences
Lähde: ORCID
Nimike
Adjunct of the Faculty of Graduate Studies 2013 -
Yksikkö
Oceanography
Lähde: ORCID
Nimike
Postdoctoral researcher 2009 - 2012
Université de Rennes 1
Yksikkö
Géosciences
Lähde: ORCID
Nimike
Postdoctoral researcher 2008 - 2009
University of Michigan
Yksikkö
Geological Sciences
Lähde: ORCID
Nimike
Research Assistant 2003 - 2008
ExxonMobil Exploration Company
Lähde: ORCID
Nimike
Geoscientist (intern) 2007 - 2007
Koulutus
Tutkinnot
B.S. 1.9.1998 - 15.12.2002 / University of Michigan
Ph.D. 1.9.2003 - 2.10.2008 / University of Michigan
Julkaisut (20)
Exploring the relationships between low-temperature thermochronometers, temperature-time histories, and geological processes using Tc1D
2023
Records of continent-continent collisions in the Paleoproterozoic: exploring the effects of convergence obliquity and temperature on P-T-t paths
2023
Megathrust Heterogeneity, Crustal Accretion, and a Topographic Embayment in the Western Nepal Himalaya: Insights from the Inversion of Thermochronological Data
2022
Rahoitusmyönnöt (3)
Termokronometrien säteilyvaurioherkkyyden hyödyntäminen kratonien paljastumishistorian määrittämisessä Suomen Akatemia2023 - 2027
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 AndesSuomen Akatemia2014 - 2018
What controls strain partitioning at obliquely convergent ocean-continent margins? 3D dynamics of crustal deformation along the western Andean marginUniversity of Helsinki Research Funds2014 - 2017