Skip to main content
Log in

Reply to Oczlon’s (2006) comment

  • Reply
  • Published:
International Journal of Earth Sciences Aims and scope Submit manuscript

Abstract

The comment of Martin Oczlon contains some significant contributions to the topics discussed in the article of Huckriede et al. (Int J Earth Sci 93:414–431, 2004). Contrary to Oczlon’s comment, the central results of Huckriede et al. (Int J Earth Sci 93:414–431, 2004) are clearly different from the tectonic model of Oczlon (Geol Rundsch 83:20–31, 1994). Additionally, there is no reason for a new interpretation of the 40K/40Ar muscovite cooling-ages from allochthonous units.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Franke W, Oncken O (1995) Zur prädevonischen Geschichte des Rhenohercynischen Beckens. Nova Acta Leopoldina NF 71:53–72

    Google Scholar 

  • Franke W, Walliser O (1983): “Pelagic” Carbonates in the Variscan Belt—their sedimentary and tectonic environments. In: Martin H, Eder FW (eds) Intracontinental fold belts. Springer, Berlin Heidelberg New York, pp 77–92

    Google Scholar 

  • Haverkamp J (1991) Detritusanalyse unterdevonischer Sandsteine des Rheinisch-Ardennischen Schiefergebirges und ihre Bedeutung für die Rekonstruktion der sedimentliefernden Hinterländer. Dissertation RWTH Aachen, 1–195

  • Huckriede H, Wemmer K, Ahrendt H (2004) Palaeogeography and tectonic structure of allochthonous units in the German part of the Rheno-Hercynian Belt (Central European Variscides). Int J Earth Sci 93:414–431

    Article  Google Scholar 

  • Kayser E (1878) Die Fauna der ältesten Devon-Ablagerungen des Harzes. Abh preuß geol LA 2/4:1–293

    Google Scholar 

  • Oczlon MS (1992) Gondwana and Laurussia before and during the Variscan Orogeny in Europe and related areas. Heidelb Geowiss Abh 53:1–56

    Google Scholar 

  • Oczlon MS (1994) North Gondwana origin for exotic Variscan rocks in the Rhenohercynian zone of Germany. Geol Rundsch 83:20–31

    Article  Google Scholar 

  • Oczlon MS (2006) Comment on: “Palaeogeography and tectonic structure of allochthonous units in the German part of the Rheno-Hercynian Belt (Central European Variscides)”. Int J Earth Sci (in press)

  • Oncken O (1997) Transformation of a magmatic arc and an orogenic root during oblique collision and its consequences for the evolution of the European Variscides (Mid-German Crystalline Rise). Geol Rundsch 86:2–20

    Article  Google Scholar 

  • Zelichowski AM (1995) Lithostratigraphy and sedimentologic-paleogeographic development: Western Pomerania. In: Zdanowski A, Zakowa H (eds) The Carboniferous System in Poland. Polish Geological Institute, Warszawa, pp 97–100

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to H. Huckriede.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Huckriede, H., Wemmer, K. Reply to Oczlon’s (2006) comment. Int J Earth Sci (Geol Rundsch) 96, 785–787 (2007). https://doi.org/10.1007/s00531-006-0125-3

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00531-006-0125-3

Keywords

Navigation