Gentbrugge Formation
Encyclopedia
The Gentbrugge Formation ' onMouseout='HidePop("32171")' href="/topics/Gentbrugge">Gentbrugge
in East-Flanders) is a geologic formation in the west of Belgium
. The formation crops out
in East- and West-Flanders and also occurs in the subsurface
of the province of Antwerpen. It consists of marine
clay
, silt
and sand
, deposited in the shallow sea that covered northern Belgium during the Ypresian
age (around 50 million years ago, part of the early Eocene
).
The Gentbrugge Formation reaches its greatest thickness in the north of Belgium, where it can be maximally 50 meters thick. It is subdivided into three members. The base of the formation is formed by silty clay and clayey silt (Merelbeke Member). On top of this are laminae of silt (Pittem Member) and beds of very fine sand, disturbed by bioturbation
(Vlierzele Member). The sands can have horizontal bedding as well as cross bedding, and are often lithified
into sandstone
.
The Gentbrugge Formation is part of the Ieper Group
and is stratigraphically on top of the older Tielt Formation
(marine silt and sand), another formation of the same group
. On top of the Gentbrugge Formation are deposits of the Lutetian
Zenne Group
. In the north of Belgium this is often the Aalter Formation
(marine clays and sands). In the south the Aalter Formation often lacks and the younger Brussel Formation
(marine sand and marl
) and Lede Formation
(marine calcareous sand) can be found directly on top of the Gentbrugge Formation.
(eds.); 2001: Paleogene and Neogene lithostratigraphic units (Belgium), Geologica Belgica 4(1-2), p. 135-152.
Gentbrugge
Gentbrugge is one of 25 districts of the city of Ghent, Belgium in the Flemish Region of Belgium. Gentbrugge together with Oud Gentbrugge had been a separate municipality before January 1, 1977, when it fused with Ghent.- Neighborhoods :...
in East-Flanders) is a geologic formation in the west of Belgium
Belgium
Belgium , officially the Kingdom of Belgium, is a federal state in Western Europe. It is a founding member of the European Union and hosts the EU's headquarters, and those of several other major international organisations such as NATO.Belgium is also a member of, or affiliated to, many...
. The formation crops out
Outcrop
An outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. -Features:Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by a mantle of soil and vegetation and cannot be...
in East- and West-Flanders and also occurs in the subsurface
Subsurface
Subsurface is the seventh studio album by British progressive metal band Threshold. The album was released in August 2004, and received an Album of the Month award in several European music magazines....
of the province of Antwerpen. It consists of marine
Marine (ocean)
Marine is an umbrella term. As an adjective it is usually applicable to things relating to the sea or ocean, such as marine biology, marine ecology and marine geology...
clay
Clay
Clay is a general term including many combinations of one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure.- Formation :Clay minerals...
, silt
Silt
Silt is granular material of a size somewhere between sand and clay whose mineral origin is quartz and feldspar. Silt may occur as a soil or as suspended sediment in a surface water body...
and sand
Sand
Sand is a naturally occurring granular material composed of finely divided rock and mineral particles.The composition of sand is highly variable, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal...
, deposited in the shallow sea that covered northern Belgium during the Ypresian
Ypresian
In the geologic timescale the Ypresian is the oldest age or lowest stratigraphic stage of the Eocene. It spans the time between and , is preceded by the Thanetian age and is followed by the Eocene Lutetian age....
age (around 50 million years ago, part of the early Eocene
Eocene
The Eocene Epoch, lasting from about 56 to 34 million years ago , is a major division of the geologic timescale and the second epoch of the Paleogene Period in the Cenozoic Era. The Eocene spans the time from the end of the Palaeocene Epoch to the beginning of the Oligocene Epoch. The start of the...
).
The Gentbrugge Formation reaches its greatest thickness in the north of Belgium, where it can be maximally 50 meters thick. It is subdivided into three members. The base of the formation is formed by silty clay and clayey silt (Merelbeke Member). On top of this are laminae of silt (Pittem Member) and beds of very fine sand, disturbed by bioturbation
Bioturbation
In oceanography, limnology, pedology, geology , and archaeology, bioturbation is the displacement and mixing of sediment particles and solutes by fauna or flora . The mediators of bioturbation are typically annelid worms , bivalves In oceanography, limnology, pedology, geology (especially...
(Vlierzele Member). The sands can have horizontal bedding as well as cross bedding, and are often lithified
Diagenesis
In geology and oceanography, diagenesis is any chemical, physical, or biological change undergone by a sediment after its initial deposition and during and after its lithification, exclusive of surface alteration and metamorphism. These changes happen at relatively low temperatures and pressures...
into sandstone
Sandstone
Sandstone is a sedimentary rock composed mainly of sand-sized minerals or rock grains.Most sandstone is composed of quartz and/or feldspar because these are the most common minerals in the Earth's crust. Like sand, sandstone may be any colour, but the most common colours are tan, brown, yellow,...
.
The Gentbrugge Formation is part of the Ieper Group
Ieper Group
The Ieper Group is a group of rock strata in the subsurface of northwest Belgium. The group is subdivided into three marine formations, all formed during the Ypresian, a single age of the geologic timescale...
and is stratigraphically on top of the older Tielt Formation
Tielt Formation
The Tielt Formation is a geologic formation in the subsurface of Belgium. The formation crops out in the north of Hainaut, in the southern and central parts of West- and East-Flanders and in Walloon and Flemish Brabant...
(marine silt and sand), another formation of the same group
Group (stratigraphy)
A group in stratigraphy is a lithostratigraphic unit, a part of the geologic record or rock column that consists of defined rock strata. Groups are divided into formations and are sometimes themselves grouped into "supergroups"....
. On top of the Gentbrugge Formation are deposits of the Lutetian
Lutetian
The Lutetian is, in the geologic timescale, a stage or age in the Eocene. It spans the time between and . The Lutetian is preceded by the Ypresian and is followed by the Bartonian. Together with the Bartonian it is sometimes referred to as the Middle Eocene subepoch...
Zenne Group
Zenne Group
The Zenne Group is a group of rock strata in the subsurface of central and northwest Belgium. The group consists of three formations, all from the Ypresian and Lutetian ages...
. In the north of Belgium this is often the Aalter Formation
Aalter Formation
The Aalter Formation is a geologic formation in the subsurface of northwest Belgium. The formation consists of marine clay and sand, deposited in the shallow sea thet covered northern and central Belgium in the Eocene epoch....
(marine clays and sands). In the south the Aalter Formation often lacks and the younger Brussel Formation
Brussel Formation
The Brussel Formation is a geologic formation in the subsurface of central Belgium. The formation is named after the Belgian capital, Brussels. It consists of shallow marine sandstone and calcareous sands, deposited in the sea that covered Belgium 45 million years ago, in the Eocene.The Brussel...
(marine sand and marl
Marl
Marl or marlstone is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and aragonite. Marl was originally an old term loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay...
) and Lede Formation
Lede Formation
The Lede Formation is a geologic formation in the subsurface of Belgium. The formation is named after the town of Lede in East Flanders. It consists of shallow-marine limestone and sandstone, deposited in the former sea that covered Belgium during the Eocene....
(marine calcareous sand) can be found directly on top of the Gentbrugge Formation.
(eds.); 2001: Paleogene and Neogene lithostratigraphic units (Belgium), Geologica Belgica 4(1-2), p. 135-152.