Geodynamic implications derived from Numidian‐like distal turbidites deposited along the Internal–External Domain Boundary of the Betic Cordillera (S Spain). (21st November 2012)

• Record Type: Journal Article
• Authors: Alcalá, Francisco J.; Guerrera, Francesco; Martín‐Martín, Manuel; Raffaelli, Giuliana; Serrano, Francisco
• Is Part Of: Terra nova. Volume 25:Number 2(2013:Apr.)
• Page Start: 119
• Page End: 129
• Publication Date: 2012-11-21
• Subjects: Earth sciences -- Periodicals; Geology -- Periodicals; 550
• DOI: 10.1111/ter.12014
• Languages: English
• ISSNs: 0954-4879

Abstract

<abstract abstract-type="main" xml:lang="en"> <title> <x xml:space="preserve">Abstract</x> </title> <sec id="sec-sum-1" sec-type="section"> <p>Terra Nova, 00, 1–12, 2012</p> </sec> <sec id="abs1-1" sec-type="section"> <title>Abstract</title> <p>New data reveal Early Burdigalian 'Numidian‐like lithofacies' in successions of the internal (southernmost) part of the South Iberian Margin (<italic>SIM</italic>) and the south‐western margin of the Mesomediterranean Microplate (<italic>MM</italic>). The well‐known Numidian Formation was deposited in the external (Massylian) sub‐domain of the Maghrebian Flysch Basin (a south‐western branch of the Tethys Ocean). The anomalous occurrence of 'Numidian‐like lithofacies' is induced by the particular Early Miocene palaeogeographical and geodynamic complexity of the sector. This consisted of a 'triple point' with a dextral transform fault between the <italic>SIM</italic> and the <italic>MM‐</italic>Maghrebian Flysch Basin system. In this framework, the ageing of Iberian reliefs and the <italic>MM</italic> collapse, coupled with an African Margin upbulging, and a shortening of the Maghrebian Flysch Basin (both related to the subduction), could have resulted in the arrival of the Numidian depositional system from so far away.</p> </sec> </abstract>