REVIEWED SCIENTIFIC PAPERS
  1. Hartz, E.H., Kristiansen, S.N., Calvert, A, Hodges, K.V., & Heeremans, M., 2006, Structural, thermal and rheological control of the Late Paleozoic basins in East Greenland., Proceedings of the Fourth International Conference on Arctic Margins, 58-76
  2. Hartz, E.H. & Hartz, V., 2003, How perfect is the Himalayan Arc?: Comment, Geology, 31, 287
  3. Hartz, E.H., Eide, E.A., Midtbøe, P., Andresen, A, Hodges, K.V., & Kristiansen, S.N., 2002 40Ar/39Ar geochronology and structural analysis:  Basin evolution and detrital feedback mechanisms, Hold with Hope region, East Greenland, Norwegian Journal of Geology, 82 (4), 341-358
  4. Hartz, E.H, Martins, M.W, Andresen, A., & Andersen, T.B., 2002, Volcanic rocks in the Devonian Solund basin, Western Norway: large landslides of Silurian (439 Ma) rhyolites, J. Geol. Soc., London, 159, 121-128
  5. Hartz, E.H. & Torsvik, T.H., 2002, Baltica upside-down: A new plate tectonic model for Rodinia and the Iapetus Ocean, Geology, 30, 255-258
  6. Hartz, E.H, Andresen, A., Martins, M.W. & Hodges K.V., 2001, Syn-contractional extension and exhumation of deep crustal rocks in the East Greenland Caledonides, Tectonics, 20, 58-78
  7. Knudsen, T.-L., Griffin, W.L. Hartz, E.H., Jackson, S.E. and Andresen, A., 2001, In situ hafnium and lead isotope analyses of detrital zircons from the Devonian sedimentary basin of NE Greenland: A record of repeated crustal reworking, Contributions to Mineralogy and Petrology., 141, 83-94
  8. Hartz, E.H., 2000, Early Syndepositional tectonics of East Greenland’s Old Red Sandstone basin, Geol. Soc. London, Spec. Publ., 180, 537-555
  9. Hartz, E.H, Andresen, A., Hodges K.V. & Martin, M.W., 2000, The Fjord Region Detachment Zone: A long-lived extensional fault in the East Greenland Caledonides, J. Geol. Soc. London, 158, 795-810
  10. Hoffman, P.F. & Hartz, E.H. 1999, A large coherent submarine landslide associated with Pan-African foreland flexure, Geology, 27, 687-690
  11. Andresen, A. & Hartz, E.H., 1998, Basement-cover relationships and orogenic evolution in the central East Greenland Caledonides, Geologiska Föreningen i Stockholm Förhandlingar 120, 191-198
  12. Hartz, E.H., Torsvik, T.H. & Andresen, A., 1998, Reply to comment: A Carboniferous age for the East Greenland “Devonian” basin: Paleomagnetic and isotopic constraints on age, stratigraphy and platereconstructions, Geology, 26, 285-6
  13. Andresen, A., Hartz, E.H. & Vold, J., 1998, A late orogenic extensional origin for the infracrustal gneiss domes of the East Greenland Caledonides (72o-74oN), Tectonophysics 285, 353-369.
  14. Hartz, E.H & Andresen, A., 1997, From collision to collapse: Complex strain permutations in the hinterland of the Scandinavian Caledonides, Jour. Geophys. Research - Solid Earth, 102, 24,697-24,712
  15. Hartz, E.H., Torsvik, T.H. & Andresen, A., 1997, A Carboniferous age for the East Greenland “Devonian” basin: Paleomagnetic and isotopic constraints on age, stratigraphy and plate-reconstruction’s,  Special  report: Geology, 25, 675-8
  16. Hartz, E.H. & Andresen, A., 1996, Reply to comment on: Caledonian sole thrust of central East Greenland: A crustal-scale Devonian extensional detachment?, Geology, 24, 472-473
  17. Hartz, E.H. , Osmundsen, P.T. & Andresen, A., 1996, Structural control of the Devonian basin in the East Greenland Caledonides, Geologiska Föreningen i Stockholm Förhandlingar 118, 37-38
  18. Andresen, A., Vold, J. & Hartz, E.H., 1996, The Fjord Region Detachment - A regional extensive mid-crustal extensional shear zone it the East Greenland Caledonides, Geologiska Föreningen i Stockholm Förhandlingar 188, 30
  19. Hartz, E.H. & Andresen, A., 1995. Caledonian sole thrust of central East Greenland: A crustal-scale Devonian extensional detachment?, Geology, 23, 637-640
  20. Andresen, A., Steen, Ø. & Hartz, E.H., 1995, Internal strain in rotated fault blocks, Profit Project Summary Reports, Reservoir Characterization Near Well Flow, Norwegian Petroleum Dir., 43-58
  21. Hartz, E.H., Andresen, A. & Andersen T.B., 1994, Structural observations adjacent to a large scale extensional detachment zone in the hinterland of the Norwegian Caledonides, Tectonophysics, 231, 123-137
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