Search Results - "BLACKBOURN, Graham"
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Heavy Oils and Oil Sands: Global Distribution and Resource Assessment
Published in Acta geologica Sinica (Beijing) (01-02-2019)“…Global recoverable resources of heavy oil and oil sands have been assessed by CNPC using a geology‐based assessment method combined with the traditional…”
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Contourite depositional system after the exit of a strait: Case study from the late Miocene South Rifian Corridor, Morocco
Published in Sedimentology (01-12-2021)“…Idealized facies of bottom current deposits (contourites) have been established for fine‐grained contourite drifts in modern deep‐marine sedimentary…”
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SOUTH CAUCASUS PALAEOGEOGRAPHY AND PROSPECTIVITY: ELEMENTS OF PETROLEUM SYSTEMS FROM THE BLACK SEA TO THE CASPIAN
Published in Journal of petroleum geology (01-07-2021)“…Nine Mesozoic and Cenozoic palaeogeographic maps are presented to illustrate the petroleum prospectivity of the South Caucasus from a fresh perspective and as…”
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RESERVOIR CHARACTERIZATION OF THE PLIOCENE RED SERIES, LAM FIELD AND SURROUNDING AREAS, OFFSHORE WESTERN TURKMENISTAN
Published in Journal of petroleum geology (01-01-2023)“…The sedimentology, petrography and reservoir potential of Pliocene sandstones within the Upper Red Series in the offshore LAM field, Western Turkmenistan, have…”
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BITUMEN RESOURCES OF THE EAST SIBERIAN BASIN
Published in Journal of petroleum geology (01-04-2023)“…The so‐called East Siberian “Basin” extends over an ancient continental block, the Siberian Platform, and is made up of a number of smaller‐scale basement…”
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EXPLORATION PLAYS IN THE CAUCASUS REGION
Published in Journal of petroleum geology (01-07-2021)“…Exploration efforts around the Greater Caucasus region started towards the end of the 19th century and established a wide range of petroleum play types in…”
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Evolution of turbidity currents deduced from extensive thin turbidites; Marnoso Arenacea Formation (Miocene), Italian Apennines
Published in Journal of sedimentary research (01-03-2007)“…Previous work has shown that large-volume (>100 km3) turbidity currents are capable of depositing extensive (>100 km) turbidites in non-channelized settings…”
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