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Comments on the paper "A crustal-upper mantle model for southeastern Sicily (Italy) from the integration of petrologic and geophysical data" by Manuella et al. (2013)
被引:6
|作者:
Beccaluva, Luigi
[1
]
Bianchini, Gianluca
[1
]
Coltorti, Massimo
[1
]
机构:
[1] Univ Ferrara, Dipartimento Fis & Sci Terra, I-44100 Ferrara, Italy
关键词:
Hyblean area;
Basic volcanism;
Xenoliths;
Petrological data;
Tectono-magmatic model;
IBLEAN VOLCANISM;
MAGMA GENERATION;
BENEATH;
COMPONENTS;
XENOLITHS;
RIFT;
D O I:
10.1016/j.jog.2013.06.005
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
The paper "A crustal-upper mantle model for southeastern Sicily (Italy) from the integration of petrologic and geophysical data" by Manuella et al. (2013) speculatively proposes that the basement beneath southeastern Sicily is made up of a fossil oceanic crust of Permo-Triassic age. The Authors support their hypothesis discussing the geochemical features of Cenozoic basic lavas and entrained xenoliths. Unfortunately, the paper does not include fundamental references on the subject, and these omissions limit the discussion of alternative hypotheses. In this reply we highlight that the new model proposed by the Authors is poorly constrained and that their argumentations are weak and sometimes wrongly founded. (C) 2013 Elsevier Ltd. All rights reserved.
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页码:58 / 60
页数:3
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