The Mineral Evolution database is currently under development.
The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.
Locality Name:Krøderen Lake, Krødsherad, Buskerud, NorwayOldest recorded age at locality: 1270Youngest recorded age at locality: 880mindat Locality ID: 284159mindat URL:http://www.mindat.org/loc-284159.htmlTectonic Settings: Total number of sublocalities beneath "Krøderen Lake, Krødsherad, Buskerud, Norway": 1Total number of bottom-level sublocalities: 1Number of Child Localities: 1Child Localities:Bjertnes PegmatiteLatitude: 60°10'18"NLongitude: 9°39'10"EDecimal Degree (lat, lon): 60.171666666667,9.6527777777778
A
This mineral is Anthropogenic.
G
This mineral is directly dated.
B
This mineral is reported as having this age.
Y
This mineral is using an age reported as an element mineralization period.
O
This mineral is using an age calculated from all data at the locality.
R
The age displayed for this mineral originates from a different, non-child locality.
P
The age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.
This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.Elements at this locality, including sub-localities: AlBeCCaCeCuHKMoNaOPPbSSiUYElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
The Pb/Pb and Pb/U ages for the sample taken from the Bjertnes Pegmatite were concordant with themselves and were described in the literature as being similar in age to other volcanic rocks of the area.
The Pb/Pb and Pb/U ages for the sample taken from the Bjertnes Pegmatite were concordant with themselves and were described in the literature as being similar in age to other volcanic rocks of the area.
The Pb/Pb and Pb/U ages for the sample taken from the Bjertnes Pegmatite were concordant with themselves and were described in the literature as being similar in age to other volcanic rocks of the area.
The Thorium age is described in the literature as being the least reliable or the most discordant ages and does not constitute a serious objection to the ~950 Ma age given by the other results.