- Tytuł:
-
Materia organiczna łupków kambru, ordowiku i syluru w basenie bałtycko-podlasko-lubelskim Polski
Organic matter in Cambrian, Ordovician and Silurian shales of the Baltic-Podlasie-Lublin Basin in Poland - Autorzy:
-
Karcz, P.
Janas, M. - Powiązania:
- https://bibliotekanauki.pl/articles/2075498.pdf
- Data publikacji:
- 2016
- Wydawca:
- Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
- Tematy:
-
materia organiczna
Formacja Piaśnica
Formacja Sasino
Formacja Udal
ogniwo Jantaru
Formacja Pelplin
skała Eval
TOC
organic matter
Piaśnica Formation
Sasino Formation
Udal Formation
Jantar Member
Pelplin Formation
Rock Eval - Opis:
- The upper Cambrian-Silurian Piaœnica, Sasino, Udal and Pelplin formations and the Jantar Member include the most organic-rich lower Paleozoic sedimentary rocks in the Baltic-Podlasie-Lublin Basin in Poland. These rocks vary significantly in terms of vertical and lateral organic matter distribution. Generally, the siltstones, mudstones, claystones and shales are characterized by TOC values from 0.1 to as much as 17.4 wt. %. Typically, the maximum TOCvaluesreachabout9wt.%.Rock-Eval,organicmatterpetrologyandbiomarkersdataclearly indicate dominance of type II kerogen. Thermal maturity of organic matter of these rocks is variable and depends mainly on the burial history and depth. In the western slope of the East-European Craton the petroleum prospective formations are located throughout the whole spectrum of thermal maturity zones, from the immature zone (eastern margin of the formations occurrence), through the oil, condensate and gas windows, to the overmature zone dominated by exhausted source rocks in the western margins of the study area.
- Źródło:
-
Przegląd Geologiczny; 2016, 64, 12; 995--999
0033-2151 - Pojawia się w:
- Przegląd Geologiczny
- Dostawca treści:
- Biblioteka Nauki
Artykuł