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Scientist Dr. rer. nat. 1992, Bochum, Germany Curator: mineral and rock collection. Tel. +49 (0)234 / 32 - 23520 Room- No: NA 03/ 174 |
1. Tilton, G.R., Schreyer, W. & Schertl, H.P. (1990): Pb-Sr-Nd-Isotopic behaviour of deeply subducted crustal rocks from the Dora Maira Massif, Western Alps, Italy: The age of the Ultrahigh-pressure metamorphism. EOS 71, p.1708.
2. Tilton, G.R., Schreyer, W. & Schertl, H.P. (1989): Pb-Sr-Nd-Isotopenverhalten von tief subduzierten Krustengesteinen aus dem Dora-Maira-Massiv, italienische Westalpen. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol. 1, p. 187.
3. Schreyer, W., Tilton, G.R. & Schertl, H.-P. (1990) Toward a P-T-time path for the pyrope-coesite rocks of the Dora Maira Massif, Western Alps. Abstract Vol. GV-Tagung: Crustal dynamics pathways and records, p. 32
4. Schertl, H.-P. & Schreyer, W. (1991): Hochdruckminerale als Einschlüsse in Schwermineralen aus der Coesit-führenden Einheit des Dora-Maira-Massivs und ihre petrologische Aussagekraft. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol. 3, p. 228.
5. Hammerschmidt, K., Schertl, H.P., Friedrichsen, H. & Schreyer, W. (1992): Überschuß-Argon während der retrograden Metamorphose der Ultrahochdruck-Gesteine des Dora Maira Massivs, italienische Westalpen. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol. 4, p. 112.
6. Hammerschmidt, K., Schertl, H.-P., Friedrichsen, H. & Schreyer, W. (1993): Überschuss-Argon in den Ultrahochdruck-Gesteinen des Dora Maira Massivs, Italienische Westalpen. GV-Tagung.
7. Schertl, H.-P. (1993): Geochemie einer Ultrahochdruck-metamorphen Gesteinsserie von Parigi, Dora-Maira Massiv/Westalpen. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol.5: p. 254.
8. Schertl, H.-P., Hammerschmidt, K., Tilton, G. & Schreyer, W. (1993): Problems and progress in the study of the ultrahigh-pressure (UHP) rocks of the Dora Maira Massif/Western Alps. TERRA abstracts, supplement No. 4 to TERRA nova 5.
9. Gebauer, D., Tilton, G.R., Schertl, H.-P. & Schreyer, W. (1993): Eocene/oligocene ultrahigh pressure (UHP)-metamorphism in the Dora Maira Massif (Western Alps) and ist geodynamic implications. TERRA abstracts, supplement No. 4 to TERRA nova 5: p. 10-11.
10. Schertl, H.-P., Grevel, C., & Schreyer, W. (1994): New geochemical and petrological data on UHPM rocks of the Dora Maira Massif. 1 st workshop on UHP metamorphism and tectonics. Abstract Vol., p. A-5.
11. Hammerschmidt, K., Schertl, H.-P., Friedrichsen, H. & Schreyer, W. (1995): Excess argon a common feature in ultrshigh-presssure rocks: a case study on micas from the Dora Maira Massif, Western Alps, Italy. TERRA abstracts, abstract supplement No. 1 to TERRA nova, Vol. 7, p. 349.
12. Grevel, C. & Schertl, H.-P. (1995): Geochemsitry and possible protoliths of teh coesite-bearing pyrope quartzites and related rocks of the southern Dora-Maira Massif, Western Alps. Goldschmidt Conference, Journal of Conference Abstracts Vol. 1(1), p. 216.
13. Schertl, H.-P. & Schreyer, W. (1996): Geochemistry and possible protoliths of coesite-bearing pyrope quartzites and related rocks from the Dora Maira Massif/Western Alps. Supplement to EOS, Transactions, AGU Vol. 77, No. 46, p. F762.
14. Schertl, H.-P., Tilton, G., Gebauer, D., Hammerschidt, K., Brix, M. & Schreyer, W. (1997): P-T-t-path of an UHP-metamorphic rock association of the Dora-Maira Massif. Abstract supplement No. 1 to TERRA nova, Vol. 9: p 32.
15. Schertl, H.-P. (1998) The coesite-bearing pyrope-quartzites and related rocks from the Dora Maira Massif: PTt-evolution and geochemsitry. International Symposium on Problems of Petrology of Magmatic and Metamorphic Rocks. Abstract Vol., p. 78-79.
16. Nowlan, U, Schertl, H.-P. & Schreyer, W. (1998): P-T evolution from the coesite-bearing unit of the southern Dora Maira Massif, Western Alps. International Workshop on UHP Metamorphism and Exhumation, Abstract Vol., p. A200-A203.
17. Krebs, M, Maresch, W.V., Schertl, H.-P.& Draper, G (1999): P-T-Pfade von Hochdruckgesteinen aus dem Rio San Juan Komplex (nördliche Dominikanische Republik). Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol. 11: p. 137
18. Schertl, H.-P., Neuser, R.D. & Sobolev, N.V. (1999): Cathodoluminescence petrography of UHP-metamorphic rocks: a useful tool in conjunction with EMS analyses. 4 th International Ecolgite Field Symposium, Abstract Vol., p. 21-22.
19. Krebs, M, Schertl, H.-P., Maresch, W.V., Gerya, T. & Draper, G. (2000): PT-paths as constraints for numerical modelling: the Rio San Juan complex, Dominican Republic. Profil, Vol. 18: p. 30.
20. Langenhorst, F., Schertl, H.-P., Schreyer, W. & Sobolev, N.V. (2001); Metamorphic diamonds from Erzgebirge and Kokchetav: Microstructural clues to their genesis. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol.. 13: p. 109.
21. Krebs, M, Gerya, T.V., Maresch, W.V., Schertl, H.-P. Stöckhert, B. & Draper, G. (2001): Serpentinite melanges of the northern Carribean: records of complex material flow in subduction zone. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol.. 13: p. 104.
22. Schertl, H.-P., Neuser, R.D. & Sobolev, N.V (2001): Cathodoluminescence provides essential information on internal structures of rock-forming minerals. International Conference on Cathodoluminescence in Geosciences, Freiberg, Abstract Vol., Cathodoluminescence in geosciences: new insights from CL in combination with other techniques.
23. Langenhorst, F, Schertl, H.-P., Schreyer, W., Sobolev, N.V. & Shatsky, V.S. (2001): Microstructural genetic fingerprints of metamorphic and other diamonds: a comparative TEM study. UHPM Workshop „Fluid/slab/mantle interactions and Ultrahigh-P minerals“, Tokyo, Abstract Vol., p. 58-60.
24. Nowlan, E.U., Schertl, H.-P. & Schreyer, W. (2001): Eclogites of the coesite bearing Brossasco-Isasca uni, Dora Maira Massif: major-, minor-, and trace element geochemistry and possible protolith. 6 th International Eclogite Conference, Niihama, Japan, Abstract Vol., p. 102-103.
25. Krebs, M., Gerya, T.V., Maresch, W.V., Schertl, H.-P., Stöckhert, B. & Draper, G. (2001): Serpentinite melanges of the northern Caribberan: records of complex material flow in a subduction zone. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol.. 13: p. 104.
26. Likhanov, I.I., Polyansky, O.P., Reverdatto, V.V., Maresch, W.V., Schertl, H.-P., Krebs, M. & Memmi, I. (2002): Micro- to macroscale interactions between deformational and metamorphic processes in Al- and Fe-rich metapelites during thrust loading (Yenisey Ridge, Russia).
27. Langenhorst, F, Schertl, H.-P., Schreyer, W., Sobolev, N.V. & Shatsky, V.S. (2002): Defect microstructures as genetic fingerprint of diamonds. 9 th International Symposium on Experimental Mineralogy, Petrology and Geochemistry, Zürich, Abstract Vol., p. 62-63.
28. Maresch, W.V., Gerya, T.V., Krebs, M., Schertl, H.-P. & Draper, G. (2002): The serpentinite melanges of the Rio San Juan Complex, Dominican Republic, and the dynamics of subduction zones. 16 th Caribbean Geological Conference, Barbados, 2002, Abstracts Vol., p. 93.
29. Schertl, H.-P., Neuser, R.D., Sobolev, N.V. & Shatsky, V.S. (2002): UHP-metamorphic rocks from Dora Maira/Western Alps, Kokchetav/Kazakhstan: New insights using cathodoluminescence petrography. Proceedings for International Workshop on Geophysics & Structure Geology of UHPM terranes, Beijing, China, p. 118-120.
30. Likhanov, I.I., Polyansky, O.P. Reverdatto, V.V., Maresch, W.V., Schertl, H.-P., Krebs, M. & Memmi, I. (2002): Micro- to macroscale interactions between deformational and metamorphic processes in Al- and Fe-rich metapelites during thrust loading (Yenisey Ridge, Russia). 18 th General Meeting of the International Mineralogical Association, Edinburgh, Scotland. Abstract Vol. “Mineralogy for the New Millennium” p. 222.
31. Maresch, W.V., Stanek, K.-P., Grafe, F., Idleman, B., Baumann, A., Krebs, M., Schertl, H.-P. & Draper, G. (2003): Age systematics of high-pressure metamorphism in the Caribbean: confronting existing models with new data. Memorias Geomin, V Congreso de Geología y Minería, La Habana, ISBN 959-7117-11-8, 39.
32. Krebs, M., Maresch, W.V., Schertl, H.-P., Baumann, A., Münker, C., Trapp, E., Gerya, T.V. & Draper, G. (2003): Geochronology and petrology of high-pressure metamorphic rocks of the Rio San Juan Complex, northern Dominican Republic. Terra Nostra 2/2003, 18. Geow. Lateinamerika-Koll., Freiberg, p. 49.
33. Perchuk, A.L., Vielzeuf, D., Schertl, H.-P., Burchard, M., Maresch, W.V., Bernhardt, H.-J. & Gerya, T.V. (2003): Fe-Mg interdiffusion in garnet: Testing a new experimental method. European Geophysical Society, Nice, 2003, Geophysical Research Abstr., Vol. 5, p. 02326.
34. Perchuk, A.L., Maresch, W.V., Schertl, H.-P. & Burchard, M. (2003): Microstructures caused by melting of metamorphic garnets. NGU Report 2003.055, Geological Survey of Norway, Eclogite Field Symopsium, Abstr. Volume, p. 110-111.
35. Schertl, H.-P., Neuser, R.D., Sobolev, N.V. & Shatsky, V.S. (2003): Cathodoluminescence petrography of UHP-metamorphic rocks from Dora Maira/Western Alps, Kokchetav/Kazakhstan and Sulu /China. NGU Report 2003.055, Geological Survey of Norway, Eclogite Field Symopsium, Abstr. Volume, p. 129-130.
36. Krebs, M., Schertl, H.-P., Maresch, W.V., Trapp, E., Baumann, A. & Draper, G. (2003): Geochemistry and petrology of high-pressure metamorphic rocks of the Rio San Juan Complex, northern Dominican Republic. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral., Vol. 15: p. 108.
37. Perchuk, A.L., Schertl, H-P., Burchard, M., Gerya, T.V., Maresch, W.V., Vielzeuf, D, Bernhardt, H-J. (2003): Diffusivity of Fe, Mg and Mn in garnet: multi-couple experiments. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral. Vol. 15: p. 146.
38. Schertl, H.-P., Neuser, R.D., Sobolev, N.V. & Shatsky, V.S. (2003): Kathodolumineszenz (KL)-Untersuchungen an UHP-Metamorphiten von Dora Maira/Westalpen, Kokchetav/Kazakhstan und der Sulu-Region/China. Ber. Dtsch. Min. Ges., Beih. z. Eur. J. Mineral. Vol. 15: p. 170.
39. Mosenfelder, J & Schertl, H.-P. (2003): Fluid infiltration and the preservation of coesite. Geol. Soc. Am., Vol. 35, No. 6: p. 225.
40. Sobolev, N.V., Schertl, H.-P., Neuser, R.D. & Shatsky, V.S. (2004): Significance of carbonate-garnet-clinopyroxene metasedimentary ultrahigh pressure rocks in Kokchetav Massif, Kazakhstan. 32nd International Geological Congress.