Fabric evolution at basement–cover interfaces in a fold-and-thrust belt and implications for décollement tectonics (Autochthon, Lower Allochthon, central Scandinavian Caledonides)

Author:

Angerer Thomas,Greiling Reinhard O.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference132 articles.

1. Anderson MW, Morris A (2004) The puzzle of axis-normal magnetic lineations in folded low-grade sediments (Bude Formation, SW England). In: Martín-Hernández F, Lüneburg M, Aubourg C, Jackson M (eds) Magnetic fabric: methods and applications. Geol Soc Lond Spec Publ 238:37–47

2. Andersson A, Dahlman B, Gee DG, Snäll S (1985) The Scandinavian alum shales. Sver Geol Unders Ser Ca 56:1–50

3. Angerer T (2007) Fossil palaeoweathering profiles and their relation to deformation at basement–cover-interfaces. Case studies from Israel, Sweden and Spain. PhD thesis, Ruprecht-Karls-University, Heidelberg pp 1–223

4. Angerer T, Greiling RO, Avigad D (2011) Fabric development in a weathering profile at a basement–cover interface, the sub-Cambrian peneplain, Israel: implications for décollement tectonics. J Struct Geol 33:819–832

5. Aranguren A, Cuevas J, Tubia JM (1996) Composite magnetic fabrics from S–C mylonites. J Struct Geol 18:863–869

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