Joyashish Thakurta

Photo of Joyashish Thakurta
Joyashish Thakurta
Assistant Professor of Geosciences
(269) 387-3667
(269) 387-5513
1123 Rood Hall, Mail Stop 5241
Mailing address: 
Department of Geosciences
Western Michigan University
1903 W Michigan Ave
Kalamazoo MI 49008-5241 USA
  • Ph.D., Indiana University, 2008
  • M.S., University of Wisconsin, 2003
  • M.Sc., Jadavpur University, 2000
  • B.Sc., University of Calcutta, 1998
Research interests: 
  • Origin of magmatic and hydrothermal sulfide mineral deposits
  • Origin of Ural-Alaskan type complexes
  • Economic mineral deposits in the Upper Peninsula of Michigan

Dr. Joyashish Thakurta is assistant professor of igneous petrology and economic geology in the Department of Geosciences at Western Michigan University. Thakurta focuses his research on the origin of magmatic intrusive bodies and the occurrences of magmatic and hydrothermal sulfide mineral deposits of base and precious metals associated with such intrusions. He emphasizes the economic importance of Ural-Alaskan type complexes and its origin. He works on the petrogenesis and geochemical characterization of a selected group of Ural-Alaskan type complexes in southeastern Alaska. Thakurta is interested in the metallic sulfide mineral deposits located in the Upper Peninsula of Michigan related to the Penokean orogeny (1.8 Ga) and the magmatic events associated with the formation of the Mid-continent Rift system (1.1 Ga). He is also interested in applications of stable isotope geochemistry in high temperature geological processes. He operates a Delta-V isotope ratio mass-spectrometer in his lab for the collection of stable isotope data.

Selected peer-refereed publications:

  • Thakurta, J., Ripley, E.M. and Li, C. (2014), Platinum group element geochemistry of sulfide-rich horizons in the Ural-Alaskan type ultramafic complex of Duke Island, southeastern Alaska, Economic Geology, vol. 109, 643-659
  • Su, B.X., Qin, K.Z., Zhou, M.F, Sakyi, P.A., Thakurta, J., Tang, D.M., Liu, P.P., Xiao, Q.H and Sun, H. (2014), Petrological, geochemical and geochronological constraints on the origin of the Xiadong Ural-Alaskan type complex in NW China and tectonic implication for the evolution of southern Central Asian Orogenic Belt, Lithos, vol. 200-201, 226-240,doi: 10.1016/j.lithos.2014.05.005
  • Li, C., Ripley, E.M., Thakurta, J., Stifter, E. and Liang, Q. (2013), Variations of highly chalcophile elements in arc ultramafic cumulates, Alaska: Subarc mantle signature and the effects of Pt-alloy and sulfide segregation during magma evolution, Chemical Geology, vol. 351, 15-28
  • Li, C., Thakurta, J. and Ripley, E.M. (2011), Low-Ca content and kink-banded texture are not unique for mantle olivine: evidence from the Duke Island Complex, Alaska; Mineralogy and Petrology, vol. 104, 147-153, DOI 10.1007/s00710-011-0188-0
  • Thakurta, J., Ripley, E.M. and Li, C. (2009)  Oxygen isotopic variability associated with multiple stages of serpentinization, Duke Island Complex, southeastern Alaska, Geochimica et Cosmochimica Acta, vol. 73, 6298-6312
  • Thakurta, J., Ripley, E.M. and Li, C. (2008a) Geochemical constraints on the origin of sulfide mineralization in the Duke Island Ultramafic Complex, southeastern Alaska, Geochemistry Geophysics Geosystems, vol. 9, Q07003, doi: 10.1029/2008GC001982                                                                        
  • Thakurta, J., Ripley, E.M. and Li, C. (2008b) Prerequisites for sulfide-poor PGE and sulfide-rich Cu-Ni-PGE mineralization in Alaskan-type complexes, Orthomagmatic ore deposits, Journal of the Geological Society of India, vol. 72, 611-622
  • Ripley, E.M., Li, C. and Thakurta, J.(2005): Magmatic Cu-Ni-PGE mineralization at a convergent plate boundary: Preliminary mineralogic and isotopic studies of the Duke Island Complex, Alaska, in Mineral Deposit Research: Meeting the Global Challenge, editors: Mao and Bierlein, Springer Berlin Heidelberg, doi: 10.1007/3-540-27946-6, 49-51