Inhaltsbereich
Publications
(Co) Author: Schulze, A.
(since 1996) [ All ]
| Paper (ISI journals) [23] |
Paper (further journals) [6] |
Chapter in Book [3] |
Conference Paper [69] |
Report [2] |
Miscellaneous [2] |
All [105] |
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(2012): Near-surface properties of an active fault derived by joint interpretation of different geophysical methods - the Arava/ Araba Fault in the Middle East. Near Surface Geophysics, 10, 5, 381-390.
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(2010): Tomographic P-wave velocity and vertical velocity gradient structure across the geothermal site Gross Schoenebeck (NE German Basin): Relationship to lithology, salt tectonics, and thermal structure. Journal of Geophysical Research, Vol. 115, B08312.
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(2010): Microseismicity induced during fluid-injection: A case study from the geothermal site at Groß Schönebeck, North German Basin. Acta Geophysica, 58, 6, 995-1020.
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(2010): Exploring the Groß Schönebeck (Germany) geothermal site using a statistical joint interpretation of magnetotelluric and seismic tomography models. Geothermics, 39, 1, 35-45.
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(2010): Correction to 'Anatomy of the Dead Sea Transform from lithospheric to microscopic scale'. Reviews of Geophysics, 48, RG1003.
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(2009): Anatomy of the Dead Sea transform from lithospheric to microscopic scale. Reviews of Geophysics, 47, RG2002.
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(2008): The reflection seismic survey of project TIPTEQ - the inventory of the Chilean subduction zone at 38.2° S. Geophysical Journal International, 172, 2, 565-571.
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(2007): Shallow architecture of the Wadi Araba fault (Dead Sea Transform) from high–resolution seismic investigations. Tectonophysics, 432, 1-4, 37-50.
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(2007): Initial results from wide-angle seismic refraction lines in the southern Cape. South African Journal of Geology, 110, 2-3, 407-418.
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(2006): Crustal structure across the Colorado Basin, offshore Argentina. Geophysical Journal International, 165, 3, 850-864.
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(2005): Seismic Detection Limits of Small, Deep, Man-Made Reflectors: A Test at a Geothermal Site in Nothern Germany. Bulletin of the Seismological Society of America, 95, 4, 1567-1573.
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(2004): The crustal structure of the Dead Sea Transform. Geophysical Journal International, 156, 3, 655-681.
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(2003): Classification of lithology from seismic tomography, a case study from the Messum igneous complex, Namibia.. Journal of Geophysical Research, 108, B3.
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(2003): Along-strike variations of crustal reflectivity related to the Andean subduction process. Geophysical Research Letters, 30, 4, 1160.
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(2001): VRANCEA99 - the crustal structure beneath the southeastern Carpathians and the Moesian Platform from a seismic refraction profile in Romania. Tectonophysics, 340, 3-4, 233-256.| EDOC: 2790 | Abstract |
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(2001): Crustal structure of the eastern Dabie Shan interpreted from deep reflection and shallow tomographic data. Tectonophysics, 333, 3-4, 347-359.
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(2000): Deep structure of the Namibia continental margin as derived from integrated geophysical studies. Journal of Geophysical Research, 105, B11, 25829-25853.| EDOC: 1874 |
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(1999): Seismic reflection image revealing offset of Andean subduction-zone earthquake locations into oceanic mantle. Nature, 397, 341-344.| EDOC: 1929 | 10.1038/16909 |
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(1999): Two-dimensional velocity models ot the Nazca plate subduction zone between 19.5°S and 25°S from wide-angle seismic measurements during the CINCA95 project. Journal of Geophysical Research, 104, 4, 7293-7317.| EDOC: 1938 | Abstract |
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(1999): The crustal structure beneath the Central Andean forearc and magmatic arc as derived from seismic studies - the PISCO 94 experiment in northern Chile (21° - 23°S). Journal of South American Earth Sciences, 237-260.| EDOC: 1942 | Abstract |
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(1999): Deep structure of the southern Ural mountains as derived from wide-angle seismic data. Geophysical Journal International, 137, 501-515.| EDOC: 1945 | Abstract |
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(1998): The refraction seismic experiment GRANU95 in the Saxothuringian belt, southeastern Germany. Geophysical Journal International, 133, 245-259.| EDOC: 1949 | Abstract |
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(1996): Crustal root beneath the Urals: Wide–angle seismic evidence. Science, 274, no. 5285, 222-224.


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