OR/14/028 Model limitations - Revision history

Dbk at 09:54, 10 August 2015

2015-08-10T09:54:33Z

← Older revision		Revision as of 10:54, 10 August 2015
Line 8:		Line 8:

	As part of the modelling process, crossovers may occur between the surfaces. Some of these are directly the result of contours overlapping in vertical space. These have been resolved wherever possible but still may exist in some places.		As part of the modelling process, crossovers may occur between the surfaces. Some of these are directly the result of contours overlapping in vertical space. These have been resolved wherever possible but still may exist in some places.

			==Reference==


	[[category: OR/14/028 Metadata report for the Weald Basin 1:250 000 resolution geological model \| 08]]		[[category: OR/14/028 Metadata report for the Weald Basin 1:250 000 resolution geological model \| 08]]

Dbk at 09:54, 10 August 2015

2015-08-10T09:54:21Z

← Older revision		Revision as of 10:54, 10 August 2015
Line 5:		Line 5:
	The Top Penarth Group surface was constructed from isopach values. Values were gridded in Arc GIS and then added to the Top Variscan Basement surface to produce depth values. The depth values were then exported and used in the modelling process as normal.		The Top Penarth Group surface was constructed from isopach values. Values were gridded in Arc GIS and then added to the Top Variscan Basement surface to produce depth values. The depth values were then exported and used in the modelling process as normal.

	The Isle of Wight monocline is presumed to be unfaulted for Cretaceous and younger rocks. More recent studies have shown this not to be the case (Evans et al., 2011)		The Isle of Wight monocline is presumed to be unfaulted for Cretaceous and younger rocks. More recent studies have shown this not to be the case (Evans et al., 2011<ref name="Evans">EVANS, D J, KIRBY, G A, and HULBERT, A G. 2011. New insights into the structure and evolution of the Isle of Wight Monocline. ''Proceedings of the Geologist's Association''. </ref>)

	As part of the modelling process, crossovers may occur between the surfaces. Some of these are directly the result of contours overlapping in vertical space. These have been resolved wherever possible but still may exist in some places.		As part of the modelling process, crossovers may occur between the surfaces. Some of these are directly the result of contours overlapping in vertical space. These have been resolved wherever possible but still may exist in some places.

Dbk: Protected "OR/14/028 Model limitations" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]

2015-06-12T07:40:08Z

Protected "OR/14/028 Model limitations" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]

← Older revision	Revision as of 08:40, 12 June 2015
(No difference)

Dbk: Created page with "notoc {{OR/14/028}} The modelled surfaces were directly constructed from the structural contours from the Weald Report and then warped to fit borehole data points (not usi..."

2015-06-12T07:39:58Z

Created page with "__notoc__ {{OR/14/028}} The modelled surfaces were directly constructed from the structural contours from the Weald Report and then warped to fit borehole data points (not usi..."

New page

__notoc__
{{OR/14/028}}
The modelled surfaces were directly constructed from the structural contours from the Weald Report and then warped to fit borehole data points (not using the Structural modelling workflow).

The Top Penarth Group surface was constructed from isopach values. Values were gridded in Arc GIS and then added to the Top Variscan Basement surface to produce depth values. The depth values were then exported and used in the modelling process as normal.

The Isle of Wight monocline is presumed to be unfaulted for Cretaceous and younger rocks. More recent studies have shown this not to be the case (Evans et al., 2011)

As part of the modelling process, crossovers may occur between the surfaces. Some of these are directly the result of contours overlapping in vertical space. These have been resolved wherever possible but still may exist in some places.

[[category: OR/14/028 Metadata report for the Weald Basin 1:250 000 resolution geological model | 08]]

OR/14/028 Model limitations - Revision history

Dbk at 09:54, 10 August 2015

Dbk at 09:54, 10 August 2015

Dbk: Protected "OR/14/028 Model limitations" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]

Dbk: Created page with "__notoc__ {{OR/14/028}} The modelled surfaces were directly constructed from the structural contours from the Weald Report and then warped to fit borehole data points (not usi..."

Dbk: Created page with "notoc {{OR/14/028}} The modelled surfaces were directly constructed from the structural contours from the Weald Report and then warped to fit borehole data points (not usi..."