Djupadal Formation
http://dbpedia.org/resource/Djupadal_Formation an entity of type: SpatialThing
The Djupadal Formation is a geologic formation in Skåne County, southern Sweden. It is Early Jurassic (probably Pliensbachian-Toarcian, or Late Toarcian) in age. It is part of the Central Skåne Volcanic Province, know by the discovery of basalt tuff layers, including , and Djupadal. An original analysis of the location of Korsaröd led to a Toarcian-Aalenian age, but was dismissed in 2016, when a series of Palynogical samples recovered a Late Pliensbachian and probably Lower Toarcian age for the Korsaröd Outcrop. The same year this result was also challenged by an in-depth study of the Lilla Hagstad neck that yield a Late Toarcian Age. The formation was deposited in the Central Skane region, linked to the late early Jurassic volcanism. The Korsaröd member includes a volcanic-derived Lagers
rdf:langString
rdf:langString
Djupadal Formation
rdf:langString
Djupadal Formation
xsd:float
55.97999954223633
xsd:float
13.63000011444092
xsd:integer
65729935
xsd:integer
1121111886
rdf:langString
Sapropel at Sandåkra
rdf:langString
Cuaternary Sediments
xsd:integer
2001
rdf:langString
Latest Pliensbachian- Latest Toarcian
rdf:langString
~(A Volcanic neck suggest 176.7 ± 0.5 Ma, Late Toarcian Age)
rdf:langString
right
<second>
600.0
<second>
3.15576E8
xsd:integer
0
rdf:langString
Marble Terrace in Waimangu Volcanic Valley.jpg
rdf:langString
Puy de Pariou 2001-07-30.jpg
rdf:langString
Puy de mercoeur dome.jpg
rdf:langString
Korsaröd Lagerstätten Location
rdf:langString
Toarcian
xsd:integer
2
rdf:langString
Central Skåne County
rdf:langString
Up to
xsd:integer
350
xsd:string
55.98 13.63
rdf:langString
The Djupadal Formation is a geologic formation in Skåne County, southern Sweden. It is Early Jurassic (probably Pliensbachian-Toarcian, or Late Toarcian) in age. It is part of the Central Skåne Volcanic Province, know by the discovery of basalt tuff layers, including , and Djupadal. An original analysis of the location of Korsaröd led to a Toarcian-Aalenian age, but was dismissed in 2016, when a series of Palynogical samples recovered a Late Pliensbachian and probably Lower Toarcian age for the Korsaröd Outcrop. The same year this result was also challenged by an in-depth study of the Lilla Hagstad neck that yield a Late Toarcian Age. The formation was deposited in the Central Skane region, linked to the late early Jurassic volcanism. The Korsaröd member includes a volcanic-derived Lagerstatten with exceptional fern finds. The data provided by fossilized wood rings showed that the location of Korsaröd hosted a middle-latitude Mediterranean-type biome in the late Early Jurassic, with low rainfall ratio, delayed to seasonal events. Superimposed on this climate were the effects of a local active and hydrothermal activity.
rdf:langString
Carita Augustsson
rdf:langString
Djupadalsmölla, Ljungbyhed
rdf:langString
Sandstone, Clay and Conglomerate
rdf:langString
Höör Sandstone, Brandsberga and Kolleberga erratics and Sapropel at Sandåkra
rdf:langString
Approx. 35°N
rdf:langString
Basalt Tuff, Veined Gneiss
xsd:nonNegativeInteger
116800
<Geometry>
POINT(13.630000114441 55.979999542236)
