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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
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
The most characteristics feature of carbonate rocks in the Transvaal Supergroup are:
Dolomites
Interbeds of Banded Iron Formations
Stromatolites
Dolomites
Interbeds of Banded Iron Formations
Stromatolites
Sedimentation of the Transvaal Supergroup was terminated by the orogenesis:
Kheis
Ubedian
Kibara
Ubedian
In the Limpopo orogenic belt region, the following is/are exposed on the surface:
The root zone of the orogen
Rocks of the continental crust
A set of nappes
The root zone of the orogen
The age of the Uberian orogenic belt is:
1950Ma
2050Ma
1800Ma
1800Ma
The Waterberg Group contains rocks that are the oldest:
Gold-bearing strata
Red-beds
BIF
Red-beds
Amalgamation of the Rodinia Supercontinent is dated at:
1000Ma
2000Ma
1600Ma
1000Ma
The Lufilian Arc (orogenic belt) of Central Africa:
Contains huge Cu-deposits
Belongs to the Pan-African orogenic belts systems
Contains glacial sediments of the Snowball Earth
Contains huge Cu-deposits
Belongs to the Pan-African orogenic belts systems
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 Arabian Craton coints mainly:
Mesoproterozoic Basement rocks
Archacan Basement rock
Pan-African island arc rock complexes
Archacan Basement rock
Pan-African island arc rock complexes
The Tippecanoe Sequence in N America is:
Its covered by the Kaskaskia Sequence
Rests unconformably on nacient continental basement
Of the age Ordovivian-Silurian
Its covered by the Kaskaskia Sequence
Of the age Ordovivian-Silurian
The Taconian Orogenesis is:
Of the Ordovivian age
Resulted from collision continent-island arc
Resulted from diachronous collision
Of the Ordovivian age
Resulted from collision continent-island arc
The famous Castkill Delta originated:
During the Arcadian orogenesis
During the Alleghenian orogenesis
Is a part of the Kaskaskia sequence
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
Asia is located on plates:
5
4
6
6
The Norilsk deposit is related to:
Eruption of the Siberian Traps
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 High Himalaya contain rocks:
Related to the Tethys Ocean
Flysch with volcanic rocks
The Gondwana formations
Related to the Tethys Ocean
In the zone of the Caledonian foldin in the NW Europe, the folds:
Are genetically related to the collision between Baltica with Laurentia
Extend NW-SE
Extend NE-SW
Are genetically related to the collision between Baltica with Laurentia

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