File:YGS CHR 01 REGI FIG 06.jpg - Revision history

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2019-08-17T20:07:04Z

Scotfot uploaded a new version of File:YGS CHR 01 REGI FIG 06.jpg

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2019-07-28T17:49:58Z

← Older revision		Revision as of 18:49, 28 July 2019
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	\|date=2019-07-27 13:46:46		\|date=2019-07-27 13:46:46
	\|source=Yorkshire Geological Society		\|source=Yorkshire Geological Society
	\|author=~~Yorkshire Geological Society~~		\|author=K. W. Glennie
	\|permission=		\|permission=
	\|other versions=		\|other versions=

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2019-07-27T12:53:31Z

← Older revision		Revision as of 13:53, 27 July 2019
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	{{Information		{{Information
	\|description={{en\|1=Figure 6 Late Carboniferous, Westphalian. The west–east trending seaway of the earlier Carboniferous was replaced by a subsiding belt of equatorial swamps that were the sites of the future Coal Measures. In the late Namurian and early Westphalian, the swamps were repeatedly inundated by the sea, giving rise to the many marine bands that have been recognized from North America to Germany. Such extensive, and in many cases correlatable, horizons suggest that, although subsidence undoubtedly played a part, the driving force behind the marine flooding, possibly from the east (cf. [[:File:YGS_CHR_01_REGI_FIG_05.jpg\|(Figure 5)]]), was likely to have been the repeated melting of Gondwanan icecaps. To the east, deposition of coal-bearing strata occurred in a narrowing band in the Polish Trough and in intermontane basins such as the Saar–Nahe. Modified from Ziegler (1987).}}		\|description={{en\|1=Figure 6 Late Carboniferous, Westphalian. The west–east trending seaway of the earlier Carboniferous was replaced by a subsiding belt of equatorial swamps that were the sites of the future Coal Measures. In the late Namurian and early Westphalian, the swamps were repeatedly inundated by the sea, giving rise to the many marine bands that have been recognized from North America to Germany. Such extensive, and in many cases correlatable, horizons suggest that, although subsidence undoubtedly played a part, the driving force behind the marine flooding, possibly from the east (cf. [[:File:YGS_CHR_01_REGI_FIG_05.jpg\|(Figure 5)]]), was likely to have been the repeated melting of Gondwanan icecaps. To the east, deposition of coal-bearing strata occurred in a narrowing band in the Polish Trough and in intermontane basins such as the Saar–Nahe. Modified from Ziegler (1987).}}
			{{YGSCarbHydroRes}}
	\|date=2019-07-27 13:46:46		\|date=2019-07-27 13:46:46
	\|source=Yorkshire Geological Society		\|source=Yorkshire Geological Society

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=={{int:filedesc}}==
{{Information
|description={{en|1=Figure 6 Late Carboniferous, Westphalian. The west–east trending seaway of the earlier Carboniferous was replaced by a subsiding belt of equatorial swamps that were the sites of the future Coal Measures. In the late Namurian and early Westphalian, the swamps were repeatedly inundated by the sea, giving rise to the many marine bands that have been recognized from North America to Germany. Such extensive, and in many cases correlatable, horizons suggest that, although subsidence undoubtedly played a part, the driving force behind the marine flooding, possibly from the east (cf. [[:File:YGS_CHR_01_REGI_FIG_05.jpg|(Figure 5)]]), was likely to have been the repeated melting of Gondwanan icecaps. To the east, deposition of coal-bearing strata occurred in a narrowing band in the Polish Trough and in intermontane basins such as the Saar–Nahe. Modified from Ziegler (1987).}}
|date=2019-07-27 13:46:46
|source=Yorkshire Geological Society
|author=Yorkshire Geological Society
|permission=
|other versions=
}}

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