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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03
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Identification of uppercrustal discontinuities using dip curvature analysis of isostatic residual gravity: examples from the central Andes

Riller, UlrichORCIDiD
Götze, Hans-Joachim
Schmidt, SabineORCIDiD
Trumbull, RobertORCIDiD
Hongn, Fernado
Petrinovic, Ivan
2006
Universitätsverlag Göttingen
Article in Anthology
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Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1887
Riller, Ulrich; Götze, Hans-Joachim; Schmidt, Sabine; Trumbull, Robert; Hongn, Fernado; Petrinovic, Ivan, 2006: Identification of uppercrustal discontinuities using dip curvature analysis of isostatic residual gravity: examples from the central Andes. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 181 - 182., , DOI: 10.23689/fidgeo-1887.
 
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  • Abstract
Structural analysts are often faced with the problem of identifying prominent structural discontinuities covered by post-tectonic sedimentary or volcanic rocks. Gravity fields are often used to delineate the trace of buried discontinuities but are frequently found to be too crude to localize discontinuities adequately. Here, we introduce the importance of dip curvature of the isostatic residual gravity for identifying upper-crustal discontinuities. The relationship between Bouguer gravity, isostatic residual gravity and its dip curvature, first-order structural elements and distribution of Neogene volcanic rocks was examined in the central Andean plateau, more specifically, the southern Altiplano and the Puna...
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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Zentralanden
Erdkruste
Diskontinuität <Geologie>
Gravimetrie
Südamerika {Geophysik}
Gravimetrische Verfahren {Geophysik}
Alpidische Orogene {Geologie}
Anden {Geologie}
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