File:YGS CHR 01 REGI FIG 03.jpg - Revision history

Scotfot: Scotfot uploaded a new version of File:YGS CHR 01 REGI FIG 03.jpg

2019-08-17T19:58:19Z

Scotfot uploaded a new version of File:YGS CHR 01 REGI FIG 03.jpg

← Older revision	Revision as of 20:58, 17 August 2019
(No difference)

Scotfot: /* {{int:filedesc}} */

2019-07-28T17:47:40Z

← Older revision		Revision as of 18:47, 28 July 2019
Line 6:		Line 6:
	\|date=2019-07-27 13:32:32		\|date=2019-07-27 13:32:32
	\|source=Yorkshire Geological Society		\|source=Yorkshire Geological Society
	\|author=~~Yorkshire Geological Society~~		\|author=K. W. Glennie
	\|permission=		\|permission=
	\|other versions=		\|other versions=

Scotfot: /* {{int:filedesc}} */

2019-07-27T12:39:09Z

← Older revision		Revision as of 13:39, 27 July 2019
Line 1:		Line 1:
	=={{int:filedesc}}==		=={{int:filedesc}}==
	{{Information		{{Information
	\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [:File:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).		\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [[:File:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).

	{{YGSCarbHydroRes}}}}		{{YGSCarbHydroRes}}}}

Scotfot: /* {{int:filedesc}} */

2019-07-27T12:38:31Z

← Older revision		Revision as of 13:38, 27 July 2019
Line 1:		Line 1:
	=={{int:filedesc}}==		=={{int:filedesc}}==
	{{Information		{{Information
	\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [~~[Media~~:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).		\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [:File:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).

	{{YGSCarbHydroRes}}}}		{{YGSCarbHydroRes}}}}

Scotfot at 12:36, 27 July 2019

2019-07-27T12:36:15Z

← Older revision		Revision as of 13:36, 27 July 2019
Line 1:		Line 1:
	=={{int:filedesc}}==		=={{int:filedesc}}==
	{{Information		{{Information
	\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [[~~File~~:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).		\|description={{en\|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [[Media:YGS_CHR_01_REGI_FIG_02.jpg\|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).

	{{YGSCarbHydroRes}}}}		{{YGSCarbHydroRes}}}}

Scotfot: User created page with UploadWizard

2019-07-27T12:35:33Z

User created page with UploadWizard

New page

=={{int:filedesc}}==
{{Information
|description={{en|1=Figure 3 Mid-Devonian. Closure of the Iapetus Ocean resulted in the creation of a large Devonian (Old Red Sandstone) continent that covered eastern Laurentia–Greenland and modern Scandinavia. Scotland and England were united. Through the middle of the main Caledonian mountain range, the approximate location of parts of the Iapetus Suture can be deduced from the occurrence of intermontane basins containing both fluvial and lacustrine sedimentary sequences. Mid-Devonian marine limestones extended from the Rheic Ocean far into that continental area, suggestive of a northwest–southeast trending tensional gash orthogonal to the sharp bend in the Iapetus Suture seen so clearly on [[File:YGS_CHR_01_REGI_FIG_02.jpg|(Figure 2)]] and which possibly is also connected with the suture of the old Tornquist Sea. An active west–east trending Hercynian (Variscan) Fold Belt was developing south of the Rheic Ocean. Britain was still south of the Equator during the Devonian. Modified from Ziegler (1987).

{{YGSCarbHydroRes}}}}
|date=2019-07-27 13:32:32
|source=Yorkshire Geological Society
|author=Yorkshire Geological Society
|permission=
|other versions=
}}

=={{int:license-header}}==
{{subst:Custom license marker added by UW}}
{{YGS}}

[[Category:Uploaded with UploadWizard]]