1887

Abstract

Ordovician successions in the North Gondwana are best understood in the framework of a Lower Paleozoic development. In the Cambrian-Ordovician successions of southern Turkey (Taurus chain or Taurides, Figure 1) and SE Turkey (Border Folds of the Arabian Plate), four major depositional sequences have been defined based on recognition of major transgressive events and subsequent shelf progradations (Ghienne et al., 2010).

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/content/papers/10.3997/2214-4609-pdb.367.4
2012-09-09
2021-12-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.367.4
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