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Bradley R Hacker
University Of California-Santa Barbara
$3,692,281
Attributed
$5,571,523
Total exposure
23
Grants
21
Lead (contact PI)
Attributed= this PI's even-split share of every grant they're on (the fair, additive number). Exposure = full size of all those grants.
Funding over time
peak $1M · FY2005–19$2M$1.5M$1M$500K$0
'05
'06
'07
'08
'09
'10
'11
'12
'13
'14
'15
'16
'17
'18
'19
Funding mix
By agency
NSF$5,571,523 · 23
By mechanism
—$5,571,523 · 23
Top collaborators
- James M Mattinson4 shared
- Andrew Kylander-Clark3 shared
- John M Cottle2 shared
- James R Boles1 shared
- Matthew E Rioux1 shared
- Matthew G Jackson1 shared
- Peter B Kelemen1 shared
- Rachel M Haymon1 shared
Grant awards (23)
Collaborative Research: Dating Deformation with Titanite$289,046
· FY2019 · GEO · contact PI
Collaborative Research: How Does Lower Continental Crust Form? A Petrochronological Investigation of the Ivrea Zone$186,584
· FY2019 · GEO · contact PI
Collaborative research: Structure and dynamics of the Alaska mantle wedge$91,110
· FY2018 · GEO · contact PI
Collaborative Research: Characterizing and Modeling Crustal Recycling$332,772
· FY2016 · GEO · contact PI
MRI: Acquisition of a Thermal Ionization Mass Spectrometer (TIMS) for high-precision isotopic research of the Earth's mantle, crust and oceans$524,244
· FY2014 · GEO
What Causes UHT Metamorphism: Lengthscales and Timescales$304,644
· FY2014 · GEO · contact PI
Collaborative Research: Did the Pamir Gneiss Domes and Salient form by Northward Underthrusting of India or Southward Subduction and Rollback of Asia?$173,765
· FY2014 · GEO · contact PI
Collaborative Research: the role of fluids in intermediate-depth seismicity and wedge anisotropy: Case studies for Cascadia and Alaska, with a comparison to Japan$75,489
· FY2013 · GEO · contact PI
What Determines Whether the Deep Continental Crust Flows?$329,701
· FY2012 · GEO · contact PI
Collaborative Research: The suturing process: Insight from the India-Asia collision zone$266,136
· FY2011 · GEO
The Dynamics of UHP Tectonism: Does the Western Gneiss Region Consist of Multiple (U)HP Blocks With Different Histories?$391,382
· FY2009 · GEO · contact PI
How Does the Lower Crust Thicken and Grow During Continent Collisions? A Case Study of the Pamir$341,828
· FY2009 · GEO · contact PI
Collaborative Research: Testing Channel-flow Models Using Mid-crustal Rocks of North Himalayan Gneiss Domes$227,664
· FY2009 · GEO · contact PI
Collaborative Research: Using Mineral Physics to Interpret Seismic Anisotropy of the Basin and Range Crust$279,279
· FY2008 · GEO · contact PI
Collaborative Research: Element Recycling from UHP Metasediments: Evidence and Consequences$141,339
· FY2008 · GEO · contact PI
Collaborative Research: How Is Rifting Exhuming the Youngest High-pressure and Ultrahigh-pressure (HP/UHP) Rocks on Earth?$312,317
· FY2007 · GEO · contact PI
Acquisition of a New Electron Imaging Facility$299,745
· FY2007 · GEO · contact PI
Collaborative Research: Earthscope integrated investigation of Cascadia subduction zone tremor, structure and process$138,744
· FY2006 · GEO · contact PI
Support for the Penrose Conference on Arc Crustal Genesis and Evolution; July 9-15, 2006; Valdez, Alaska$15,000
· FY2006 · GEO · contact PI
The Assembly of UHP Terranes: Was the Western Gneiss Region Built By Sequential or Repeated (Ultra)High-Pressure Events?$328,178
· FY2005 · GEO · contact PI
Collaborative Research (USC and UCSB): Direct Observation of Depth Variation in Fault Zone Structure Through and Below the Seismogenic Crust$116,316
· FY2004 · GEO · contact PI
CSEDI: Collaborative Research: Thermal, Petrological, and Seismological Study of Subduction Zones$130,126
· FY2002 · GEO · contact PI
Collaborative Research: Subduction and Exhumation of Ultrahigh-Pressure Rocks -- Field and Drilling Studies in Eastern China$276,114
· FY2001 · GEO · contact PI