Inhaltsbereich
Publications
(Co) Author: Lucassen, F.
| Paper (ISI journals) [24] |
Paper (further journals) [2] |
Chapter in Book [5] |
Conference Paper [35] |
All [66] |
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(2013): Coupled H and Nb-, Cr-, and V trace element behavior in synthetic rutile at 600°C, 400 MPa, and possible geological application. American Mineralogist, 98, 1, 7-18.
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(2012): Small-scale transport of trace elements Nb and Cr during growth of titanite: an experimental study at 600 °C, 0.4 GPa. Contributions to Mineralogy and Petrology, 164, 6, 987-997.
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(2012): The morphology of the reaction front of the dissolution-precipitation reaction rutile + wollastonite = titanite in time series experiments at 600°C/400 MPa. American Mineralogist, 97, 5-6, 828-839.
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(2011): The Early Palaeozoic high-grade metamorphism at the active continental margin of West Gondwana in the Andes (NW Argentina/N Chile). International Journal of Earth Sciences, 100, 2-3, 445-463.
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(2011): Element and Sr isotope signatures of titanite as indicator of variable fluid composition in hydrated eclogite. Lithos, 121, 1-4, 12-24.
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(2011): Distinctive properties of rock-forming blue quartz: inferences from a multi-analytical study of submicron mineral inclusions. Mineralogical Magazine, 75, 4, 2519-2534.
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(2010): Lavas and their mantle xenoliths from intracratonic Eastern Paraguay (South America Platform) and Andean Domain, NW-Argentina: a comparative review. Mineralogy and Petrology, 98, 1-4, 143-165.
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(2010): Redistribution of HFSE elements during rutile replacement by titanite. Contributions to Mineralogy and Petrology, 160, 2, 279-295.
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(2010): Ti-Al zoning of experimentally grown titanite in the system CaO-Al2O3-TiO2-SiO2-NaCl-H2O-(F): Evidence for small-scale fluid heterogeneity. American Mineralogist, 95, 10, 1365-1378.
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(2010): Complete recycling of a magmatic arc: evidence from chemical and isotopic composition of Quaternary trench. International Journal of Earth Sciences, 99, 3, 687-701.
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(2008): Zircon geochronology and Sr, Nd, Pb isotope geochemistry of granitoids from Bayuda Desert and Sabaloka (Sudan): Evidence for a Bayudian event (920-900 Ma) preceding the Pan-African orogenic cycle (860-590 Ma) at the eastern boundary of the Saharan Metacra. Precambrian Research, 164, 1-2, 16-39.
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(2008): Late Cenozoic xenoliths as a guide to the chemical – isotopic composition and thermal state of the upper mantle under northeast Africa. European Journal of Mineralogy, 20, 6, 1079-1096.
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(2008): Nd, Pb, and Sr isotope composition of Late Mesozoic to Quaternary intra-plate magmatism in NE-Africa (Sudan, Egypt): high-μ signatures from the mantle lithosphere. Contributions to Mineralogy and Petrology, 156, 6, 765-784.
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(2007): Pre-Cenozoic intra-plate magmatism along the Central Andes (17–34°S): Composition of the mantle at an active margin. Lithos, 99, 3-4, 312-338.
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(2006): Nd, Pb, and Sr isotope composition of juvenile magmatism in the Mesozoic large magmatic province of northern Chile (1827°S): indications for a uniform subarc mantle. Contributions to Mineralogy and Petrology, 152, 5, 571-589.
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(2005): Ordovician metamorphism and plutonism in the Sierra de Quilmes metamorphic complex: Implications for the tectonic setting of the northern Sierras Pampeanas (NW Argentina). Lithos, 83, 1-2, 143-181.
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(2005): The late Cretaceous lithospheric mantle beneath the Central Andes: Evidence from phase equilibria and composition of mantle xenoliths. Lithos, 82, 3-4, 379-406.
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(2004): Distinguishing crustal recycling and juvenile additions at active continental margins: The paleozoic to Recent compositional evolution of the Chilean Pacific margin (36-41°S). Journal of South American Earth Sciences, 17, 2, 103-119.
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(2003): Chemical and Isotopic Composition of Lower to Upper Ordovician Sedimentary Rocks (Central Andes/South Bolivia): Implications for their Source. Journal of Geology, 111, 4, 487-497.| EDOC: 5840 |
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(2003): Timing of high-grade metamorphism; early Palaeozoic U-Pb formation ages of titanite indicate long-standing high-T conditions at the western margin of Gondwana (Argentina, 26-29 degrees S).. Journal of Metamorphic Geology, 21, 7, 649-662.| EDOC: 4107 |
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(2002): Isotopic composition of Late Mesozoic basic and ultrabasic rocks from the Andes (23-32°S) - Implications for their mantle sources. Contributions to Mineralogy and Petrology, 143, 3, 336-349.| EDOC: 2881 |
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(2002): Lead evolution of the Pre-Mesozoic crust in the Central Andes (18°-27°): Progressive homogenisation of Pb. Chemical Geology, 186, 3-4, 183-197.| EDOC: 2882 |
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(2001): Comment on the paper "Puncoviscana folded belt in northwestern Argentina: testimony of Late Proterozoic Rodinia fragmentation and pre-Gondwana collisional episodes" by Omarini et al.. International Journal of Earth Sciences, 90, 4, 890-893.
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(2001): Composition and density model of the continental crust at an active continental margin - the Central Andes between 21° and 27°S. Tectonophysics, 341, 195-223.
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(2000): The evolution of a continental margin from a geochemical and petrological point of view - The Central Andes (18° - 26°S). Zeitschrift für Angewandte Geologie, SH1, 317-322.| EDOC: 2041 |
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(2000): The evolution of a continental margin from a geochemical and petrological point of view. The Central Andes (18°S - 26°S). In: Miller, H. and Hervé, F. (eds,) Geoscientific Cooperation with Latin America. Zeitschrift für Angewandte Geologie, Sonderheft 1, 317-322.| EDOC: 2827 |
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(2011): Late Mesozoic to Quaternary intraplate magmatism and its relation to the Neoproterozoic lithosphere in NE Africa - New data from lower-crustal and mantle xenoliths from the Bayuda volcanic field, Sudan. - In: Beccaluva, L.; Bianchini, G.; Wilson, M. (Eds.), Volcanism and Evolution of the African Lithosphere, Geological Society of America, 1-24.
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(2006): Crustal evolution at the Central Andean continental margin: a geochemical record of crustal growth, recycling and destruction. - In: Oncken, O.; Chong, G.; Franz, G.; Giese, P.; Götze, H.-J.; Ramos, V. A.; Strecker, M. R.; Wigger, P. (Eds.), The Andes - Active Subduction Orogeny, Springer, 45-64.| EDOC: 9180 |
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(2006): Long-Term Geological Evolution and Mass-Flow Balance of the South-Central Andes. - In: Oncken, O.; Chong, G.; Franz, G.; Giese, P.; Götze, H.-J.; Ramos, V.; Strecker, M.; Wigger, P. (Eds.), The Andes - Active Subduction Orogeny, Springer, 401-428.| EDOC: 9353 |
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(2006): The Segmented Overriding Plate and Coupling at the South-Central Chilean Margin (36-42°S). - In: Oncken, O.; Chong, G.; Franz, G.; Giese, P.; Götze, H.-J.; Ramos, V.; Strecker, M.; Wigger, P. (Eds.), The Andes - Active Subduction Orogeny, Springer, 355-374.| EDOC: 9351 |
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(2005): The early Palaeozoic Orogen in the Central Andes: a non-collisional orogen comparable to the Cenozoic high plateau?. - In: Vaughan, A. P. M.; Leat, P. T.; Pankhurst, R. J. (Eds.), Terrane Processes at the Margins of Gondwana, 257-273.| EDOC: 6989 |
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(2011): Hydrogen incorporation into pure and Nb-, Cr-, V-doped synthetic rutile at 600°C, 400MPa. 7th European Conference on Mineralogy and Spectroscopy - ECMS 2011 (Potsdam, Germany 2011), 48.| EDOC: 17522 |
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(2010): 3D-view of a reaction front for a dissolution-precipitation reaction - the rutile-titanite reaction. Abstract Book, 88. Jahrestagung der Deutschen Mineralogischen Gesellschaft - From Dust to Dust - (Münster 2010).| EDOC: 15816 |
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(2010): Hydrogen incorporation in rutile - evidence from hydrothermal experiments on synthetic single-crystal rutile. Abstract Book, 88. Jahrestagung der Deutschen Mineralogischen Gesellschaft - From Dust to Dust - (Münster 2010), S06-T01.| EDOC: 15807 |
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(2008): Rutile Replacement by Titanite (I): Experimental Growth. 86. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Berlin 2008), 145.| EDOC: 11943 |
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(2008): Rutile Replacement by Titanite (II): Experimental Growth. 86. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Berlin 2008), 148.| EDOC: 11942 |
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(2007): Nd, Pb, and Sr isotope composition of Late Mesozoic to Quaternary intra - plate magmatism in NE - Africa (Sudan, Egypt): implications for the mantle sources. Vom All zum Kern : Geowissenschaften in Afrika ; Programm & Abstracts, Jahrestagung der Afrikagruppe deutscher Geowissenschaftler (Potsdam 2007), 24.| EDOC: 9960 | PDF |
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(2005): 600 Ma of crustal evolution in the Central Andes: a site of crustal growth or destruction at an active continental margin?. 6th International Symposium on Andean Geodynamics (Barcelona 2005).| EDOC: 7134 |
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(2005): Complete recycling of the magmatic arc in Chile (36° - 39°S) – evidence from chemical and isotopic composition of (sub)recent trench sediments.. 6th International Symposium on Andean Geodynamics (Barcelona 2005).| EDOC: 7135 |
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(2005): Causes and Consequences of Crustal Melting in the Central Andes. International Final Symposium of the Collaborative Research Center 'Deformation Processes in the Andes', SFB 267 (Potsdam 2005).| EDOC: 6886 |
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(2004): Upper mantle xenoliths from Central Argentine (Eastern Pampean Ranges): Geothermobarometry and isotopic data.. 32nd International Geological Congress (Florence 2004).| EDOC: 7125 |
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(2004): Cretaceous metasomatism of lithospheric mantle: Trace element and isotopic composition of spinel lherzolite xenoliths from NW Argentina.. 14th Annual Goldschmidt Conference (Copenhagen, Denmark 2004), A715.| EDOC: 7137 |
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(2003): Timing of high-grade metamorphism: Early Paleozoic U-Pb formation ages of titanite indicate long-standing high-T conditions in the southern Puna and western Sierras Pampeanas (Argentina, 26 - 29°S).. 4th South American Symposium on Isotope Geology (Salvador, Brazil 2003), 41-44.| EDOC: 7007 |
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(2003): Low temperature alteration of calc alkaline granitoids of Nahuelbuta Mountains, south-central Chile (36°30’-38.00’S).. 10th Congreso Geológico Chileno (Concepción, Chile 2003).| EDOC: 7132 |
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(2003): The occurence and thermal disequilibrium of cummingtonite in plutonic rocks of Nahuelbuta Mountains.. 10th Congreso Geológico Chileno (Concepción, Chile 2003).| EDOC: 7133 |
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(2003): Changing magma composition in the Late Paleozoic versus Early Mesozoic in the Andes – a stationary versus a moving arc?. 10° Congreso Geologico Chileno (Concepción, Chile 2003).| EDOC: 7130 |
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(2003): Early Palaeozoic high-T metamorphism and magmatism in the Central Andes: an analogy to the present high plateau?. 10th Congreso Geológico Chileno (Concepción, Chile 2003).| EDOC: 7131 |
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(2003): Sr, Nd, and Pb Isotopic composition of clinopyroxene and temperature and age of mineral equilibria: late Cretaceous mantle xenoliths from the Central Andes.. 4th South American Symposium on Isotope Geology (Salvador, Brazil 2003), 589-592.| EDOC: 7008 |
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(2003): Searching for causes of Andean segmentation (15°-47°S): interpretation of elastic thickness and isotopic data, plus a preliminary 3D density model.. 10° Congreso Geologico Chileno (Concepción, Chile 2003).| EDOC: 7129 |
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(2002): Concordant titanite U-Pb ages of Cambrian to Silurian high T metamorphism at the western edge of Gondwana (Southern Puna and western Sierras Pampeanas, Argentina, 26 - 29°S).. 5th International Symposium on Andean Geodynamics (ISAG) (Toulouse 2002), 77-80.| EDOC: 7126 |
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(2002): Petrology of the Hualpén stock: Evidence of late Triassic epizonal plutonism at the western Margin of Gondwana (36°45’S, 73°10’W).. 5th International Symposium on Andean Geodynamics (ISAG) (Toulouse 2002), 167-170.| EDOC: 7127 |
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(2002): Crustal recycling and juvenile additions: the Paleozoic to recent tectonic and compositional evolution of the Chilean continental margin (36° - 40°S). 5th International Symposium on Andean Geodynamics (ISAG) (Toulouse, France 2002), 393-396.| EDOC: 4858 |
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(2002): Mineral composition variations as effect of contact metamorphism in the metapelites of the Eastern Series, Nahuelbuta Mountains, South-Central Chile.. 5th International Symposium on Andean Geodynamics (ISAG) (Toulouse 2002), 677-680.| EDOC: 7128 |
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(2001): Ordovician basin formation by ductile thinning of high-grade metamorphic crust in the Sierras Pampeanas, NW Argentina. MARGINS Meeting (Kiel 2001).| EDOC: 4765 |
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(2001): Long-term compositional evolution of a continental margin – the Central Andes 18-27°S.. MARGINS Meeting (Kiel 2001), 126.| EDOC: 6612 |
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(2001): Sr, Nd, Pb - isotopic and geochemical composition of metasedimentary and magmatic rocks of the late Paleozoic and Mesozoic basement in Chile and W Argentina (36°30-40'S; 70°30'-73°W) - implications for the source regions of the pre-Cenozoic basement. III. South American Symposium on Isotope Geology.| EDOC: 2833 |
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(2000): Time-deformation relations of ordovician metamorphism and magmatism of the pre-Andean crust: The Sierra de Quilmes (NW Argentia). 31st International Geological Congress (Rio de Janeiro Brazil 2000).| EDOC: 4749 |
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(2000): Time-deformation relations of lower Paleozoic metamorphism and magmatism in the Sierra de Quilmes (NW Argentina). 17. Geowissenschaftliches Lateinamerika-Kolloquium (Stuttgart 2000), 43.| EDOC: 4751 |
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(2000): Composition and density of the continental crust in the Andes between 18° and 27°S. 17. LateinAmerika-Kolloquium, p. 31.| EDOC: 1830 |
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(2000): Isotopic composition of late Mesozoic mafic rocks from the Andes (23-32°S) - implications for their mantle sources. DMG, 117.| EDOC: 1719 |
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(1999): The Continental Crust of the Central Andes (21°-26°S) - The petrological - geochemical perspective. EUG 10, p. 420.| EDOC: 1617 |
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(1999): Isotopic composition of Late Mesozoic mafic rocks from the Andes (23-32°S) - how heterogeneous is the mantle source?. Fourth International Symposium on Andean Geodynamics, 454-457.| EDOC: 1749 |
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(1999): Isotopic composition of Late Mesozoic mafic rocks from the Andes (23-32°S) - how heterogeneous is the mantle source?. II South American Symposium on Isotope Geology, 238-242.| EDOC: 1914 |
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(1999): Crust-mantle mixing in continental arc magmas: Petrological and petrophysical investigations in the Andes. 24th General Assembly of the European Geophysical Society (The Hague, Netherlands 1999).| EDOC: 2285 |
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(1998): Metamorphism and composition of the Central Andean crust through time. 3rd Andean Geoscience Workshop.| EDOC: 2879 |
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(1998): Isotopic contrasts in Neogene ignimbrites from the central Andes (23°S - 27°S): source heterogeneity or different petrogenesis?. 16. Geowissenschaftliches Lateinamerika-Kolloquium, p. 152.| EDOC: 1629 |