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  <controlfield tag="008">260224s2018    xxu                 ing  </controlfield>
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    <subfield code="a">Petroleum provinces of the paratethyan region</subfield>
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    <subfield code="c">jul. 2018</subfield>
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    <subfield code="a">22/01/2019 ; 17/01/2019</subfield>
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    <subfield code="a">51 p. ; 247-298</subfield>
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    <subfield code="a">Transcripci&#xF3;n del resumen del autor: Initial crustal collision between Africa and Eurasia in the middle Eocene &amp;#x96; early Oligocene enclosed a semi-restricted Paratethyan seaway of linked basins and platforms across a region stretching from the Eastern Alps to the South Caspian Sea. As the African Plate continued to advance north during the later Neogene, the seaway shrank into a series of more isolated basins separated by the rising Alpine &amp;#x96; Carpathian &amp;#x96; Caucasus fold-thrust belts. Organic-rich oil-prone Paratethyan source rocks of middle Eocene (Kuma Formation and equivalents) and Oligocene &amp;#x96; early Miocene (Maikop and Menilite Beds) ages, and more gas prone post-orogenic midupper Miocene shales, subsequently charged over 2500 accumulations across the region with combined recoverable reserves of 95 billion brl oil-equivalent (B boe). These accumulations are clustered in discrete petroleum provinces, each with a distinct tectonostratigraphic architecture and comprised of one or more petroleum systems.</subfield>
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    <subfield code="d">2026-03-06</subfield>
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    <subfield code="r">2026-03-06 00:36:30</subfield>
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