Premium
Aeromagnetic map constrains cratonization of the Arabian Shield
Author(s) -
Nehlig Pierre,
Asfirane Fawsia,
Genna Antonin,
Guerrot Catherine,
Nicol Nadège,
Salpeteur Ignace,
Shanti Mohammed,
Thiéblemont Denis
Publication year - 2001
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1046/j.1365-3121.2001.00370.x
Subject(s) - geology , gondwana , accretion (finance) , shield , molasse , paleontology , volcano , tectonics , seismology , foreland basin , physics , astrophysics
A new aeromagnetic map together with new geological and geochronological data has led to a reinterpretation of the geological history of the Arabian Shield. The magnetic anomalies outline an orogenic complex containing a network of mostly left‐lateral strike‐slip faults, including the Nabitah Belt and several peripheral mountain ranges. Oblique accretion resulted in obliteration of early volcanic‐arc magnetic fabrics, which were almost completely replaced by a NW–SE magnetic fabric in the northern Shield; the southern Shield, however, reveals extensive E–W anomalies related to post‐accretion magmatic intrusions. This complex web of orogenic zones is intimately associated with synchronous molasse basins that formed 680–610 Ma. The distribution and chronology of orogenic zones, related to the closing of East and West Gondwana, brings into question several earlier assumptions, such as high continental growth rates, palaeogeodynamic reconstructions, the definitions of the Nabitah and Najd faults, and the significance of molasse basins.