Reply to Narkiewicz (2017) comment on "Thermal evolution of Paleozoic successions of the Holy Cross Mountains (Poland)"

• Type: Another Publication in an International Scientific Journal
• Date: 2017

Authors

Schito, A (Author) Other; Corrado, S (Author) Other; Trolese, M (Author) Other; Aldega, L (Author) Other; Caricchi, C (Author) Other; Cirilli, S (Author) Other; Grigo, D (Author) Other; Guedes, A (Author) FCUP; Spina, A (Author) Other; B. Valentim (Author) FCUP

Journal

Title: Marine and Petroleum Geology

Vol. 88

Pages: 1114-1122

ISSN: 0264-8172

Publisher: Elsevier

Indexing

ISI Web of Knowledge - 1 Citation

Scopus - 1 Citation

Other information

Authenticus ID: P-00N-C3P

DOI: 10.1016/j.marpetgeo.2017.07.018

Abstract (EN): In this paper we reply to the criticisms advanced by Narkiewicz (2017) on the paper by Schito et al. (2017). We clarify the issues related to the stratigraphic and thermal maturity constraints used for reconstructing burial and thermal models of the two blocks of the Holy Cross Mountains. We also show how geological evidences brought by Narkiewicz (2017) as a proof of elevated Variscan heat flow are not conclusive or at least suggest the occurence of a localized thermal anomaly only along the, area of the Holy Cross Fault. In the end, we performed new burial and thermal models in the Kielce region demonstrating that stratigraphic thickness variations between Schito et al. (2017) and Narkiewicz et al. (2010) produce only negligible differences in levels of thermal maturity of Paleozoic rocks. In addition, we outline that levels of thermal maturity for Silurian rocks can be matched only by using constant heat flow values through the Paleozoic and point to a decisive role for the absence of regional high Variscan heat flow in the area.

Language: English

Type (Professor's evaluation): Scientific

No. of pages: 9