Occurrences of the asphaltic substances in Southeastern Turkey and their genesis

In an area of approximately 17,200 km2 in Southeastern Turkey a prospection was carried out in all parts where occurrences of asphaltic substances could be expected in accord with the stratigraphical-tectonic situation. The author describes the vein-like occurrences, partially explored by trenches a...

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Main Author: Richard F. LEBKUCHNER
Format: Article
Language:English
Published: General Directorate of Mineral Research and Exploration 1969-01-01
Series:Bulletin of the Mineral Research and Exploration
Subjects:
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Online Access:http://dergipark.gov.tr/bulletinofmre/issue/3898/52020?publisher=mta
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spelling doaj-bfb9838ea4774ab6a6ee6dfea09cf7b22020-11-25T00:45:39ZengGeneral Directorate of Mineral Research and ExplorationBulletin of the Mineral Research and Exploration0026-45632651-30481969-01-0172727476Occurrences of the asphaltic substances in Southeastern Turkey and their genesisRichard F. LEBKUCHNERIn an area of approximately 17,200 km2 in Southeastern Turkey a prospection was carried out in all parts where occurrences of asphaltic substances could be expected in accord with the stratigraphical-tectonic situation. The author describes the vein-like occurrences, partially explored by trenches and drillings, which attain a length of up to 3500 meters (Avgamasya and Milli veins) and locally a width up to 80 m (Avgamasya vein). The author arrives at the conclusion that tectonic events, such as upthrusts and overthrusts, caused the opening of often irregular systems of deep-reaching, broad, gaping fissures. In particular, tilting of strata below the overthrusts was observed, whereas diagonal fissures are a very striking feature of the hanging parts. Soft masses of asphalt originating from a former oil horizon, intricately mixed with mineral substance, were squeezed into these fissures right up to the surface region, under the pressure of overlying rock masses. An «asphaltic pyrobituminous shale» in the «Cudi group» was recognized as one of the ancient oil horizons.http://dergipark.gov.tr/bulletinofmre/issue/3898/52020?publisher=mta---
collection DOAJ
language English
format Article
sources DOAJ
author Richard F. LEBKUCHNER
spellingShingle Richard F. LEBKUCHNER
Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
Bulletin of the Mineral Research and Exploration
-
-
-
author_facet Richard F. LEBKUCHNER
author_sort Richard F. LEBKUCHNER
title Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
title_short Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
title_full Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
title_fullStr Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
title_full_unstemmed Occurrences of the asphaltic substances in Southeastern Turkey and their genesis
title_sort occurrences of the asphaltic substances in southeastern turkey and their genesis
publisher General Directorate of Mineral Research and Exploration
series Bulletin of the Mineral Research and Exploration
issn 0026-4563
2651-3048
publishDate 1969-01-01
description In an area of approximately 17,200 km2 in Southeastern Turkey a prospection was carried out in all parts where occurrences of asphaltic substances could be expected in accord with the stratigraphical-tectonic situation. The author describes the vein-like occurrences, partially explored by trenches and drillings, which attain a length of up to 3500 meters (Avgamasya and Milli veins) and locally a width up to 80 m (Avgamasya vein). The author arrives at the conclusion that tectonic events, such as upthrusts and overthrusts, caused the opening of often irregular systems of deep-reaching, broad, gaping fissures. In particular, tilting of strata below the overthrusts was observed, whereas diagonal fissures are a very striking feature of the hanging parts. Soft masses of asphalt originating from a former oil horizon, intricately mixed with mineral substance, were squeezed into these fissures right up to the surface region, under the pressure of overlying rock masses. An «asphaltic pyrobituminous shale» in the «Cudi group» was recognized as one of the ancient oil horizons.
topic -
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url http://dergipark.gov.tr/bulletinofmre/issue/3898/52020?publisher=mta
work_keys_str_mv AT richardflebkuchner occurrencesoftheasphalticsubstancesinsoutheasternturkeyandtheirgenesis
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