and 29: REINTERPRETATION OF THE PERNÍK BED.and 27: NEW STABLE ISOTOPE DATA AND FOSSILS.
and 23: EARLY ORDOVICIAN ARTHROPOD TRACE FO.and 19: CONCLUSIONS Fossil associations of.and 17: FAUNAL TURNOVER NEAR THE KATIAN/HIR.and 15: FAUNAL TURNOVER NEAR THE KATIAN/HIR.and 11: about 10 m above the traditional Or.and 5: this is perhaps less clear in the s.Given the glacial context, it is generally assumed that erosion was associated both with tunnel valleys and ice streams. 1km to >20km, and remnant Mid-Ordovician palaeohighs.
#Canigo tucuman catalogo series#
As a whole, the uppermost Ordovician package is bounded at the base by a major unconformity defining a series of paleovalleys ranging in width from ca. In most cases subsurface biostratigraphy confirms a possible late Katian to Hirnantian age for this sequence. Sequence CO3: Is the uppermost Ordovician section assigned in Libya to the Melaz Shugran, Mamuniyat and Bir Tlacsin formations. It comprises the laterally extensive and distinctive Lower Ordovician (Tremadocian-Floian?) Achebayat Formation overlain, along a probable transgressive surface of erosion, by interbedded burrowed sandstones, cross-bedded channel-fill sandstones and mudstones of Middle Ordovician age (Dapingian-Sandbian), known as the Hawaz Formation, and interpreted as shallow-marine sediments deposited within a megaestuary or gulf. Sequence CO2: Truncates CO1 along a low angle, Type II unconformity.
It comprises the possible Upper Cambrian to Lowermost Ordovician Hassaouna Formation. 20 De Febrero, 37 is 306 meters away, 5 min walk.Pellegrini 43 is 296 meters away, 5 min walk. acepto permuta, llamame ¡Ver Detalles Fiat argo precision 1.8 nafta 2018. Tomo canje, llamame ¡Ver Detalles C3 aircross exclusive 1.6 nafta 201. 1750000 ¡Ver Detalles Toyota corolla xei 2016. STRATIGRAPHIC FRAMEWORK The uppermost Ordovician section is the youngest of three major sequences recognized widely across the entire Saharan Platform: Sequence CO1: Unconformably overlies the Precambrian or Infracambrian basement. Which Bus lines stop near Camping-Articulos-Canigo Salta sa.Salta is 2379 meters away, 31 min walk.Pellegrini 171 is 421 meters away, 6 min walk.Avenida Belgrano 635 is 378 meters away, 6 min walk.Belgrano 663 is 337 meters away, 5 min walk. Canigo en San Miguel De TucumÁn - Tucuman Tel: (0381) 421-5529 Dir: 24 De Septiembre. This paper is a brief summary of the results of fieldwork, in outcrops across SW Libya, together with the analysis of cores, hundreds of well logs (including many high quality image logs) and seismic lines focused on the uppermost Ordovician of the Murzuq Basin. This is especially so in the case of the Saharan Platform where Upper Ordovician sediments are well developed and represent a major target for hydrocarbon exploration. INTRODUCTION An Upper Ordovician glacial episode is widely recognized as a significant event in the geological history of the Lower Paleozoic. Keywords: Ordovician, Libya, glaciation, Mamuniyat, Melaz Shugran, Hirnantian. 2 REMSA, Dhat El-Imad Complex, Tower 3, Floor 9, Tripoli, Libya. Gruenwald 2 1 Repsol Exploración, Paseo de la Castellana 280, 28046 Madrid, Spain. ISBN 978-84-7840-857-3 © Instituto Geológico y Minero de España 2011 ICE IN THE SAHARA: THE UPPER ORDOVICIAN GLACIATION IN SW LIBYA – A SUBSURFACE PERSPECTIVE N.D. Instituto Geológico y Minero de España, Madrid. García-Bellido (eds.), Ordovician of the World.