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.
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: AgAlAsBaBeBiCCaCdClCuFFeHKLiMgMnMoNaNbNiOPPbSScSiSnSrThTiUYZnZrElements from minerals reported directly at this locality: Al As Bi Ca Fe H Mn O P Pb S Sc Ti Y Structural Groups for minerals in this locality:
The study area lies in the NE Bavarian crystalline basement close to the Czech-German border and covers part of the Moldanubian Zone at the western edge of the Bohemian Massif. Precambrian paragneisses were deformed during the Variscan orogeny and subsequently intruded by acidic igneous rocks of late Carboniferous age. Following these granitic intrusions, acidic differentiates, including aplites and pegmatites very different in their mineral compositions, evolved. Some are significantly enriched in Nb oxides and Li-Mn phosphates. After the Variscan orogeny, the NE Bavarian Basement was subjected to a strong uplift. In the basement proper, clastic sediments and relics of the Cenozoic regolith were locally preserved on a low-relief landscape. These relict landforms date back to the late Mesozoican and the early Cenozoic when subtropical climates occurred in what is today called the "Oberpfaelzer Wald." By the end of the glacial period, present-day fluvial drainage systems cut into the basement rocks and transported the debris of the older regolith and of lithoclasts eroded during the glacial period.
Giersdorf_00000877
The study area lies in the NE Bavarian crystalline basement close to the Czech-German border and covers part of the Moldanubian Zone at the western edge of the Bohemian Massif. Precambrian paragneisses were deformed during the Variscan orogeny and subsequently intruded by acidic igneous rocks of late Carboniferous age. Following these granitic intrusions, acidic differentiates, including aplites and pegmatites very different in their mineral compositions, evolved. Some are significantly enriched in Nb oxides and Li-Mn phosphates. After the Variscan orogeny, the NE Bavarian Basement was subjected to a strong uplift. In the basement proper, clastic sediments and relics of the Cenozoic regolith were locally preserved on a low-relief landscape. These relict landforms date back to the late Mesozoican and the early Cenozoic when subtropical climates occurred in what is today called the "Oberpfaelzer Wald." By the end of the glacial period, present-day fluvial drainage systems cut into the basement rocks and transported the debris of the older regolith and of lithoclasts eroded during the glacial period.
Giersdorf_00000878
The study area lies in the NE Bavarian crystalline basement close to the Czech-German border and covers part of the Moldanubian Zone at the western edge of the Bohemian Massif. Precambrian paragneisses were deformed during the Variscan orogeny and subsequently intruded by acidic igneous rocks of late Carboniferous age. Following these granitic intrusions, acidic differentiates, including aplites and pegmatites very different in their mineral compositions, evolved. Some are significantly enriched in Nb oxides and Li-Mn phosphates. After the Variscan orogeny, the NE Bavarian Basement was subjected to a strong uplift. In the basement proper, clastic sediments and relics of the Cenozoic regolith were locally preserved on a low-relief landscape. These relict landforms date back to the late Mesozoican and the early Cenozoic when subtropical climates occurred in what is today called the "Oberpfaelzer Wald." By the end of the glacial period, present-day fluvial drainage systems cut into the basement rocks and transported the debris of the older regolith and of lithoclasts eroded during the glacial period.
Giersdorf_00000879
The study area lies in the NE Bavarian crystalline basement close to the Czech-German border and covers part of the Moldanubian Zone at the western edge of the Bohemian Massif. Precambrian paragneisses were deformed during the Variscan orogeny and subsequently intruded by acidic igneous rocks of late Carboniferous age. Following these granitic intrusions, acidic differentiates, including aplites and pegmatites very different in their mineral compositions, evolved. Some are significantly enriched in Nb oxides and Li-Mn phosphates. After the Variscan orogeny, the NE Bavarian Basement was subjected to a strong uplift. In the basement proper, clastic sediments and relics of the Cenozoic regolith were locally preserved on a low-relief landscape. These relict landforms date back to the late Mesozoican and the early Cenozoic when subtropical climates occurred in what is today called the "Oberpfaelzer Wald." By the end of the glacial period, present-day fluvial drainage systems cut into the basement rocks and transported the debris of the older regolith and of lithoclasts eroded during the glacial period.
Giersdorf_00000880
The study area lies in the NE Bavarian crystalline basement close to the Czech-German border and covers part of the Moldanubian Zone at the western edge of the Bohemian Massif. Precambrian paragneisses were deformed during the Variscan orogeny and subsequently intruded by acidic igneous rocks of late Carboniferous age. Following these granitic intrusions, acidic differentiates, including aplites and pegmatites very different in their mineral compositions, evolved. Some are significantly enriched in Nb oxides and Li-Mn phosphates. After the Variscan orogeny, the NE Bavarian Basement was subjected to a strong uplift. In the basement proper, clastic sediments and relics of the Cenozoic regolith were locally preserved on a low-relief landscape. These relict landforms date back to the late Mesozoican and the early Cenozoic when subtropical climates occurred in what is today called the "Oberpfaelzer Wald." By the end of the glacial period, present-day fluvial drainage systems cut into the basement rocks and transported the debris of the older regolith and of lithoclasts eroded during the glacial period.