Northern Ireland Chalk nomenclature (Ulster Cretaceous Province) - Hibernian Greensands Group: Belfast Marls Formation: Difference between revisions
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Name | =====Name===== | ||
The Belfast Marls Member was first used in Griffith and Wilson (1982). The term is upgraded to formation status herein | The Belfast Marls Member was first used in Griffith and Wilson (1982). The term is upgraded to formation status herein | ||
Type section | =====Type section==== | ||
Cloghfin Port area [J 483 938] where three exposures of the formation occur, Woodburn Glen South and 503 m north-west of Knock Lodge. | Cloghfin Port area [J 483 938] where three exposures of the formation occur, Woodburn Glen South and 503 m north-west of Knock Lodge. | ||
Primary Reference Section | =====Primary Reference Section===== | ||
Carrs Glen near Belfast [J 311 793], in a borehole near Magheramorne [J 433 975]. Numerous localities on the Larne, Antrim, Carrickfergus and Belfast sheet areas (see Griffith and Wilson (1982), Page 48, Figure 16A). | Carrs Glen near Belfast [J 311 793], in a borehole near Magheramorne [J 433 975]. Numerous localities on the Larne, Antrim, Carrickfergus and Belfast sheet areas (see Griffith and Wilson (1982), Page 48, Figure 16A). | ||
=====Formal subdivisions===== | |||
Formal subdivisions | |||
None | None | ||
=====Lithology===== | |||
Lithology | |||
Pale grey strongly bioturbated silty marls with a scattering of dark green glauconite grains (not exceeding 40%). Transitional ‘zone’ at the top contains relatively little glauconite. Fossiliferous with concentrations into discreet laterally continuous shell-beds. '' '' | Pale grey strongly bioturbated silty marls with a scattering of dark green glauconite grains (not exceeding 40%). Transitional ‘zone’ at the top contains relatively little glauconite. Fossiliferous with concentrations into discreet laterally continuous shell-beds. '' '' | ||
=====Definition of upper boundary===== | |||
Definition of upper boundary | |||
Conformable, junction arbitrarily drawn at the base of the lowest persistent hard calcareous siltstone of the overlying Island Magee Siltstones Formation. This junction appears at the top of a transitional zone showing an upward decrease in glauconite content. | Conformable, junction arbitrarily drawn at the base of the lowest persistent hard calcareous siltstone of the overlying Island Magee Siltstones Formation. This junction appears at the top of a transitional zone showing an upward decrease in glauconite content. | ||
=====Definition of lower boundary===== | |||
Definition of lower boundary | |||
Unconformable, oversteps various older units.'' '' | Unconformable, oversteps various older units.'' '' | ||
=====Thickness===== | |||
Thickness | |||
Maximum thickness of a little less than 3.0m known from a borehole near Magheramorne [J 433 975] in the Larne (sheet 21) area. Minimum thickness of 1.6m over the Knockagh Axis north of Belfast. | Maximum thickness of a little less than 3.0m known from a borehole near Magheramorne [J 433 975] in the Larne (sheet 21) area. Minimum thickness of 1.6m over the Knockagh Axis north of Belfast. | ||
=====Distribution===== | |||
Distribution | |||
East Antrim Basin and Southern Uplands area of Northern Ireland. | East Antrim Basin and Southern Uplands area of Northern Ireland. | ||
=====Previous names===== | |||
Previous names | |||
Glauconitic Sands of Tate (1865) and subsequent workers. | Glauconitic Sands of Tate (1865) and subsequent workers. | ||
=====Belfast Marls Member===== | |||
=====Parent===== | |||
Parent | |||
Hibernian Greensand Group. | Hibernian Greensand Group. | ||
=====''Age and biostratigraphy''===== | |||
''Age and biostratigraphy'' | |||
Upper Cretaceous, Cenomanian. ''Mantelliceras mantelli'' to basal ''Acanthocerus rhotomagense'' Zone.'' '' | Upper Cretaceous, Cenomanian. ''Mantelliceras mantelli'' to basal ''Acanthocerus rhotomagense'' Zone.'' '' | ||
=====References===== | |||
References | |||
Griffith and Wilson (1982). | Griffith and Wilson (1982). | ||
[[category:Northern_Ireland_Chalk_nomenclature_(Ulster_Cretaceous_Province)_-_Hibernian_Greensands_Group | 01]] | [[category:Northern_Ireland_Chalk_nomenclature_(Ulster_Cretaceous_Province)_-_Hibernian_Greensands_Group | 01]] | ||
Revision as of 12:13, 21 May 2014
Name
The Belfast Marls Member was first used in Griffith and Wilson (1982). The term is upgraded to formation status herein
=Type section
Cloghfin Port area [J 483 938] where three exposures of the formation occur, Woodburn Glen South and 503 m north-west of Knock Lodge.
Primary Reference Section
Carrs Glen near Belfast [J 311 793], in a borehole near Magheramorne [J 433 975]. Numerous localities on the Larne, Antrim, Carrickfergus and Belfast sheet areas (see Griffith and Wilson (1982), Page 48, Figure 16A).
Formal subdivisions
None
Lithology
Pale grey strongly bioturbated silty marls with a scattering of dark green glauconite grains (not exceeding 40%). Transitional ‘zone’ at the top contains relatively little glauconite. Fossiliferous with concentrations into discreet laterally continuous shell-beds.
Definition of upper boundary
Conformable, junction arbitrarily drawn at the base of the lowest persistent hard calcareous siltstone of the overlying Island Magee Siltstones Formation. This junction appears at the top of a transitional zone showing an upward decrease in glauconite content.
Definition of lower boundary
Unconformable, oversteps various older units.
Thickness
Maximum thickness of a little less than 3.0m known from a borehole near Magheramorne [J 433 975] in the Larne (sheet 21) area. Minimum thickness of 1.6m over the Knockagh Axis north of Belfast.
Distribution
East Antrim Basin and Southern Uplands area of Northern Ireland.
Previous names
Glauconitic Sands of Tate (1865) and subsequent workers.
Belfast Marls Member
Parent
Hibernian Greensand Group.
Age and biostratigraphy
Upper Cretaceous, Cenomanian. Mantelliceras mantelli to basal Acanthocerus rhotomagense Zone.
References
Griffith and Wilson (1982).