Magallania

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Chemical and stable isotope composition (18O/16O, 2H/1H) of formation waters from the Carabobo Oilfield, Venezuela

T. Boschetti

B. Angulo

F. Quintero

J. Volcán

A. Casalins

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Abstract: In this short note, we present the first data on stable isotope composition of the oilfield waters from Carabobo area of the Faja Petrolífera del Orinoco “Hugo Chávez” (Orinoco Oil Belt). From a chemical point of view, the formation waters show a main Na-Cl l

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DOI: https://doi.org/10.1344/GeologicaActa2018.16.3.2

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Neogene-Quaternary onshore record in the lower Ebro river incised palaeovalley (Ebro margin, Catalan Coastal Range, NE Iberia)

A. Arasa-Tuliesa

L. Cabrera

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Abstract: The lower Ebro is a bedrock-alluvial mixed incised valley with a persistent degradational stacking architecture developed from latest Serravallian(?) to Holocene. This degradational pattern was probably controlled by isostatic rebound in NE Iberia and punctua

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DOI: https://doi.org/10.1344/GeologicaActa2018.16.3.3

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Geochemistry and petrogenesis of metabasites from the Gol-e-Gohar Complex in southern Sanandaj-Sirjan metamorphic zone, South of Iran; Evidences for crustal extension and magmatism at early Palaeozoic

H. Fatehi

H. Ahmadipour

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Abstract: In Gol-e-Gohar metamorphic Complex from south-eastern Sanandaj-Sirjan metamorphic zone (Kerman province, Iran), there are two types of metabasites, wich contain layered metamorphosed lava flows and younger meta-gabbros. The protoliths formed in the Paleozoic

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DOI: https://doi.org/10.1344/GeologicaActa2018.16.3.4

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Integrated approach for zonation of a mid-Cenomanian carbonate reservoir in a sequence stratigraphic framework

R. Jodeyri-Agaii

H. Rahimpour-Bonab

V. Tavakoli

R. Kadkhodaie-Ilkhchi

M.-R. Yousefpour

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Abstract: The mid-Cenomanian Mishrif Formation (Fm.) is considered as one of the most important rudist-bearing reservoir horizons in the Sirri Oil Fields of the Persian Gulf. Due to the general heterogeneity of carbonate reservoirs, the use of an integrated approach is

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DOI: https://doi.org/10.1344/GeologicaActa2018.16.3.5

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