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Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits

Stutenbecker, Laura ; Tollan, Peter M. E. ; Madella, Andrea ; Lanari, Pierre (2019)
Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits.
In: Solid Earth, 10 (5)
doi: 10.5194/se-10-1581-2019
Artikel, Bibliographie

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Kurzbeschreibung (Abstract)

The Neogene evolution of the European Alps was characterized by the exhumation of crystalline basement, the so-called external crystalline massifs. Their exhumation presumably controlled the evolution of relief, distribution of drainage networks, and generation of sediment in the Central Alps. However, due to the absence of suitable proxies, the timing of their surficial exposure and thus the initiation of sediment supply from these areas are poorly constrained.

The northern Alpine foreland basin preserves the Oligocene to Miocene sedimentary record of tectonic and climatic adjustments in the hinterland. This contribution analyses the provenance of 25 to 14 Myr old alluvial fan deposits by means of detrital garnet chemistry. Unusually grossular- and spessartine-rich garnet is found (1) to be a unique proxy for identifying detritus from the external crystalline massifs and (2) to occur abundantly in ca. 14 Myr old deposits of the foreland basin. In contrast to previous assumptions, we therefore propose that the external massifs were already exposed to the surface ca. 14 Myr ago.

Typ des Eintrags: Artikel
Erschienen: 2019
Autor(en): Stutenbecker, Laura ; Tollan, Peter M. E. ; Madella, Andrea ; Lanari, Pierre
Art des Eintrags: Bibliographie
Titel: Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits
Sprache: Englisch
Publikationsjahr: 2019
Verlag: Copernicus
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Solid Earth
Jahrgang/Volume einer Zeitschrift: 10
(Heft-)Nummer: 5
DOI: 10.5194/se-10-1581-2019
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Kurzbeschreibung (Abstract):

The Neogene evolution of the European Alps was characterized by the exhumation of crystalline basement, the so-called external crystalline massifs. Their exhumation presumably controlled the evolution of relief, distribution of drainage networks, and generation of sediment in the Central Alps. However, due to the absence of suitable proxies, the timing of their surficial exposure and thus the initiation of sediment supply from these areas are poorly constrained.

The northern Alpine foreland basin preserves the Oligocene to Miocene sedimentary record of tectonic and climatic adjustments in the hinterland. This contribution analyses the provenance of 25 to 14 Myr old alluvial fan deposits by means of detrital garnet chemistry. Unusually grossular- and spessartine-rich garnet is found (1) to be a unique proxy for identifying detritus from the external crystalline massifs and (2) to occur abundantly in ca. 14 Myr old deposits of the foreland basin. In contrast to previous assumptions, we therefore propose that the external massifs were already exposed to the surface ca. 14 Myr ago.

Sachgruppe der Dewey Dezimalklassifikatin (DDC): 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften
Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Angewandte Sedimentgeologie
Hinterlegungsdatum: 27 Sep 2019 06:42
Letzte Änderung: 03 Jul 2024 02:42
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