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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. und Schertl, H.-P. (1989): Pb-Sr-Nd Isotopic Behavior of Deeply Subducted Crustal Rocks from the Dora Maira Massif, Western Alps, Italy. Geochimica et Cosmochimica Acta, 53:1391-1400.
2. Schertl, H.-P., Schreyer, W. und Chopin, C. (1991): The Pyrope-Coesite Rocks and their Country Rocks at Parigi, Dora Maira Massif, Western Alps: Detailed Petrography, Mineral Chemistry and PT-Path. Contributions to Mineralogy and Petrology 108:1-21.
3. Tilton, G.R., Schreyer, W. und Schertl, H.-P. (1991): Pb-Sr-Nd Isotopic Behavior of Deeply Subducted Crustal Rocks from the Dora Maira Massif, Western Alps, Italy-II: what is the age of the Ultrahigh-Pressure Metamorphism?. Contributions to Mineralogy and Petrology 108:22-33.
4. Schertl, H.-P. und Okay, A.I. (1994): A Coesite Inclusion in Dolomite in Dabie Shan, China: Petrological and Rheological Significance. European Journal of Mineralogy 6:995-1000.
5. Chopin, C., Ferraris, G., Ivaldi, G, Schertl, H.-P., Schreyer, W., Compagnoni, R., Davidson, C. und Davis, M. (1995): Magnesiodumortierite, a new Mineral from Very-High-Pressure Rocks (Western Alps). II. Crystal Chemistry and Petrological Significance. European Journal of Mineralogy 7:525-535.
6. Grevel, C. und Schertl, H.-P. (1995): Geochemistry and possible protoliths of coesite-bearing pyrope quartzites and related rocks of the southern Dora Maira Massif, Western Alps. Bochumer Geologische und Geotechnische Arbeiten 44:60-63.
7. Gebauer, D., Schertl, H.-P. und Schreyer, W. (1995): A 35 Ma old ultrahigh-pressure metamorphism in the Dora Maira Massif and ist geodynamic implications for the Pennine zone of the Central and Western Alps. Bochumer Geologische und Geotechnische Arbeiten 44:49-53.
8. Neuser, R.D., Reinecke, T. und Schertl, H.-P. (1995): Low temperature cathodoluminescence of selected minerals from high pressure rocks. Bochumer Geologische und Geotechnische Arbeiten 44:119-123.
9. Schertl, H.-P. (1995): New petrologic observations on Dora Maira rocks: UHPM mineral inclusions in zircons and garnet-zoisite intergrowth textures. Bochumer Geologische und Geotechnische Arbeiten 44:196-199.
10. Tilton, G.R., Ames, L., Schertl, H.-P. und Schreyer, W. (1995): Age determinations on rocks of an undeformed granite contact within the coesite-bearing unit of the Dora Maira Massif. Bochumer Geologische und Geotechnische Arbeiten 44:245-247.
11. Schertl, H.-P. und Schreyer, W. (1996): Mineral Inclusions in Heavy Minerals of the Ultrahigh-Pressure Metamorphic Rocks of the Dora Maira Massif and their Bearing on the Relative Timing of the Petrological Events. Isotopic Studies of Crust-Mantle Evolution. In: A. Basu and S.R. Hart (eds.), Earth Processes: Reading the Isotopic Code, AGU, Geophysical Monograph Vol. 95:331-342.
12. Gebauer, D., Schertl, H.-P., Brix, M. und Schreyer, W. (1997): 35 Ma old Ultrahigh-Pressure Metamorphism and Evidence for Very Rapid Exhumation in the Dora Maira Massif, Western Alps. Lithos 41:5-24.
13. Tilton, G.R., Ames, L., Schertl, H.-P. and Schreyer, W. (1997): Reconnaissance Isotopic Investigations on Rocks of an Undeformed Granite Contact Within the Coesite-Bearing Unit of the Dora Maira Massif. Lithos 41:25-36.
14. Sobolev, N.V., Schertl, H.-P. und Shatsky, V.S. (1999): Some Specific Features of Carbonate-Bearing Garnet-Pyroxene Rocks. IV International Eclogite Field Symposium Russia-Kazakhstan, Field Guide Book, 33-36.
15. Chopin, C. und Schertl, H.-P. (1999): The UHP Unit in the Dora-Maira Massif, Western Alps. International Geology Review 41:765-780.
16. Nowlan, E.U., Schertl, H.-P. und Schreyer, W. (2000): Garnet-Omphacite-Phengite Thermobarometry of Eclogites from the Coesite-beraing Unit of the Dora-Maira Massif, Western Alps. Lithos 52:197-214.
17. Sobolev, N.V., Schertl, H.-P., Burchard, M. und Shatsky, V.S. (2001): An Unusual Pyrope-Grossular Garnet and its Paragenesis from Diamondiferous Carbonate-Silicate Rocks of the Kokchetav Massif, Kazakhstan. Doklady Earth Sciences 380, Nr. 7:791-794
18. Schertl, H.-P., Neuser, R.D., Sobolev, N.V. und Shatsky, V.S. (2004): UHP-metamorphic rocks from Dora Maira/Western Alps and Kokchetav/Kazakhstan: New Insights using Cathodoluminescence Petrography. European Journal of Mineralogy, 16:49-57.
19. Mosenfelder, J.L., Schertl, H.-P., Smyth, J.R. und Liou, J.G. (2004): Factors in the preservation of coesite: the importance of fluid infiltration. American Mineralogist, 90:779-789.
20. Balcázar, N., Maresch, W.V., Schertl, H.-P., Baumann, A. und Krebs, M. (2005): Petrology of the high-pressure Basal Unit, Morais Complex, NE Portugal. Indian Journal of Geology, 75:9-37.
21. Perchuk, A.L., Burchard, M., Maresch, W.V., und Schertl, H.-P. (2005): Fluid-mediated modification of garnet interiors under ultrahigh-pressure conditions. Terra Nova 17:545-553.
22. Schertl, H.-P., Medenbach, O. und Neuser, R.D. (2005): UHP-metamorphic rocks from Dora Maira, Western Alps: Cathodoluminescence of silica and twinning of coesite. Russian Geology and Geophysics, 46:1327-1332.
23. Hwang, S.-L.,, Chu H.-T., Yui, T.-F. Shen, P., Schertl, H.-P., Liou, J.G. und Sobolev, N.V. (2006): Nanometer-size P/K-rich silica glass (former melt) inclusions in microdiamond from the gneisses of Kokchetav and Erzgebirge massifs: Diversified characteristics of the formation media of metamorphic microdiamond in UHP rocks due to host-rock buffering. Earth and Planetary Science Letters 243:94-106.
24. Sobolev, N.V., Schertl, H.-P. und Neuser, R.D. (2006): Composition and paragenesis of garnets from ultrahigh-pressure calc-silicate metamorphic rocks of the Kokchetav Massif (Northern Kazakhstan). Russian Geology and Geophysics, 47:519-529.
Publikationen im Druck:
Schertl, H.-P. und Neuser, R.D. (2006): Unusual lath-shaped garnet-zoisite intergrowth textures from an UHP zoisite-quartz fels, Dora Maira: An EBSD case study. International Geology Review.
Perchuk, A.L., Burchard, M., Maresch, W.V. und Schertl, H.-P. (2006): Recycling of hydrous and carbonate mineral inclusions in garnet host under Ultrahigh pressure conditions. Lithos.
Krebs, M., Maresch, W.V., Schertl, H.-P., Baumann, A., Draper, G., Idleman, B., Münker, C. und Trapp, E. (2006): The dynamics of intra-oceanic subduction zones: A direct comparison between fossil petrological evidence (Rio San Juan Complex, Dominican Republic) and numerical simulation. Lithos.
Eingereicht:
Sobolev, N.V., Schertl, H.-P., Neuser, R.D. und Shatsky, V.S. (2006): Relics of Unusual Low Iron Pyrope-Grossular Garnets in UHPM Calc-silicate Rocks of Kokchetav Massif, Kazakhstan. International Geology Review.
Deutschsprachige Artikel:
Schertl, H.-P. und Heckmann, H. (1988): Mineralparagenese eines neuen Ferristrunzit-Vorkommens bei Wuppertal. Emser Hefte 9:35-40.
Heckmann, H. und Schertl, H.-P. (1990): Der Niederbergische Erzbergbau und seine Mineralien. Emser Hefte 11:2-40.
Schertl, H.-P. und Medenbach, O. (1994): Coesit-führender Pyrop-Quarzit – ein spektakuläres Gestein aus dem Dora-Maira Massiv in den Westalpen. Mineralienwelt Jg. 5, Nr. 1:14-16.
Homann, W., Neuser, R.D., Schertl, H.-P., Fockenberg, T und Keppler, K. (1999): Das Goldblech der Grube Ludwig im Adlersbachtal (mittlerer Schwarzwald) - eine Fälschung! Mineralienwelt Jg. 10, 5:20-23.