In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of l
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| - Coal measures (en)
- Karbon produktywny (pl)
- Вугленосна товща (uk)
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| - Karbon produktywny – tradycyjna, górnicza nazwa zespołu skał górnego karbonu Europy i Ameryki Północnej, charakteryzującego się wysoką węglonośnością. (pl)
- Вугленосна товща (рос. угленосная толща, англ. coal measures, coal-bearing strata; нім. Kohlengebirge n, Kohlengestein m, Kohlenmittel n) — комплекс , що містить в собі вугільні пласти. Вугленосна товща — умовне поняття, яке використовується при розвідці і геол.-пром. оцінці вугільних род., при характеристиці їх вугленосності і гірничо-геологічних умов розробки. Включає іноді повністю малопотужну вугленосну формацію, здебільшого — найпродуктивнішу частину розрізу потужних вугленосних формацій. (uk)
- In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of l (en)
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| - In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age. Within the Pennine Basin these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thickest development. The coal measures formed during Westphalian and earliest Stephanian times in the European ('Heerlen') chronostratigraphical scheme (which is approximately equivalent to the Middle Pennsylvanian Series of the IUGS global chronostratigraphical scheme). (en)
- Karbon produktywny – tradycyjna, górnicza nazwa zespołu skał górnego karbonu Europy i Ameryki Północnej, charakteryzującego się wysoką węglonośnością. (pl)
- Вугленосна товща (рос. угленосная толща, англ. coal measures, coal-bearing strata; нім. Kohlengebirge n, Kohlengestein m, Kohlenmittel n) — комплекс , що містить в собі вугільні пласти. Вугленосна товща — умовне поняття, яке використовується при розвідці і геол.-пром. оцінці вугільних род., при характеристиці їх вугленосності і гірничо-геологічних умов розробки. Включає іноді повністю малопотужну вугленосну формацію, здебільшого — найпродуктивнішу частину розрізу потужних вугленосних формацій. (uk)
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