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The Glossopteris Flora occurs in the following continents:
S America, N America, Europe
Africa, India, Australia
Australia, Antarctica, S America
Africa, India, Australia
Australia, Antarctica, S America
The Glossopteris Flora occurs in the following continents:
S America, N America, Europe
Africa, India, Australia
Australia, Antarctica, S America
Which observations provided the evidence for migration of the oceanic crust into the mantle:
Discovery of the Benioff Zone
Identification of volcanic island arcs
Belts od volcanoes on continental margins
Discovery of the Benioff Zone
Which observations provided the evidence for migration of the oceanic crust into the mantle:
Discovery of the Benioff Zone
Identification of volcanic island arcs
Belts od volcanoes on continental margins
The most characteristics feature of carbonate rocks in the Transvaal Supergroup are:
Dolomites
Stromatolites
Interbeds of Banded Iron Formations
Dolomites
Stromatolites
Interbeds of Banded Iron Formations
The most characteristics feature of carbonate rocks in the Transvaal Supergroup are:
Dolomites
Stromatolites
Interbeds of Banded Iron Formations
Sedimentation of the Transvaal Supergroup was terminated by the orogenesis:
Ubedian
Kibara
Kheis
Ubedian
Sedimentation of the Transvaal Supergroup was terminated by the orogenesis:
Ubedian
Kibara
Kheis
In the Limpopo orogenic belt region, the following is/are exposed on the surface:
The root zone of the orogen
A set of nappes
Rocks of the continental crust
The root zone of the orogen
In the Limpopo orogenic belt region, the following is/are exposed on the surface:
The root zone of the orogen
A set of nappes
Rocks of the continental crust
The age of the Uberian orogenic belt is:
2050Ma
1950Ma
1800Ma
1800Ma
The age of the Uberian orogenic belt is:
2050Ma
1950Ma
1800Ma
The Waterberg Group contains rocks that are the oldest:
BIF
Red-beds
Gold-bearing strata
Red-beds
The Waterberg Group contains rocks that are the oldest:
BIF
Red-beds
Gold-bearing strata
Amalgamation of the Rodinia Supercontinent is dated at:
1600Ma
2000Ma
1000Ma
1000Ma
Amalgamation of the Rodinia Supercontinent is dated at:
1600Ma
2000Ma
1000Ma
The Lufilian Arc (orogenic belt) of Central Africa:
Belongs to the Pan-African orogenic belts systems
Contains huge Cu-deposits
Contains glacial sediments of the Snowball Earth
Belongs to the Pan-African orogenic belts systems
Contains huge Cu-deposits
The Lufilian Arc (orogenic belt) of Central Africa:
Belongs to the Pan-African orogenic belts systems
Contains huge Cu-deposits
Contains glacial sediments of the Snowball Earth
The succession of the Karoo Supergroup and is lateral equivalents originated:
In the southern hemisphere
After Gondwana assembly
At passive margin
After Gondwana assembly
The succession of the Karoo Supergroup and is lateral equivalents originated:
In the southern hemisphere
After Gondwana assembly
At passive margin
The Arabian Craton coints mainly:
Pan-African island arc rock complexes
Archacan Basement rock
Mesoproterozoic Basement rocks
Pan-African island arc rock complexes
Archacan Basement rock
The Arabian Craton coints mainly:
Pan-African island arc rock complexes
Archacan Basement rock
Mesoproterozoic Basement rocks
The Tippecanoe Sequence in N America is:
Rests unconformably on nacient continental basement
Of the age Ordovivian-Silurian
Its covered by the Kaskaskia Sequence
Of the age Ordovivian-Silurian
Its covered by the Kaskaskia Sequence
The Tippecanoe Sequence in N America is:
Rests unconformably on nacient continental basement
Of the age Ordovivian-Silurian
Its covered by the Kaskaskia Sequence
The Taconian Orogenesis is:
Resulted from collision continent-island arc
Of the Ordovivian age
Resulted from diachronous collision
Resulted from collision continent-island arc
Of the Ordovivian age
The Taconian Orogenesis is:
Resulted from collision continent-island arc
Of the Ordovivian age
Resulted from diachronous collision
The famous Castkill Delta originated:
During the Alleghenian orogenesis
During the Arcadian orogenesis
Is a part of the Kaskaskia sequence
During the Arcadian orogenesis
Is a part of the Kaskaskia sequence
The famous Castkill Delta originated:
During the Alleghenian orogenesis
During the Arcadian orogenesis
Is a part of the Kaskaskia sequence
The following is/are linked with the Rocky Mountains Orogenesis:
Absence of igneous rocks
Steep subduction
Igneous rocks
Steep subduction
Igneous rocks
The following is/are linked with the Rocky Mountains Orogenesis:
Absence of igneous rocks
Steep subduction
Igneous rocks
Asia is located on plates:
4
6
5
6
Asia is located on plates:
4
6
5
The Norilsk deposit is related to:
Metamorphic remobilisation of the metals
Postmagmatic fluids
Eruption of the Siberian Traps
Eruption of the Siberian Traps
The Norilsk deposit is related to:
Metamorphic remobilisation of the metals
Postmagmatic fluids
Eruption of the Siberian Traps
The time when collision between India and Eurasia begun is:
55Ma
40Ma
45Ma
55Ma
The time when collision between India and Eurasia begun is:
55Ma
40Ma
45Ma
The High Himalaya contain rocks:
Related to the Tethys Ocean
Flysch with volcanic rocks
The Gondwana formations
Related to the Tethys Ocean
The High Himalaya contain rocks:
Related to the Tethys Ocean
Flysch with volcanic rocks
The Gondwana formations
In the zone of the Caledonian foldin in the NW Europe, the folds:
Extend NE-SW
Are genetically related to the collision between Baltica with Laurentia
Extend NW-SE
Are genetically related to the collision between Baltica with Laurentia
In the zone of the Caledonian foldin in the NW Europe, the folds:
Extend NE-SW
Are genetically related to the collision between Baltica with Laurentia
Extend NW-SE
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