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Ilość pytań: 20 Rozwiązywany: 2067 razy
The Glossopteris Flora occurs in the following continents:
S America, N America, Europe
Australia, Antarctica, S America
Africa, India, Australia
Australia, Antarctica, S America
Africa, India, Australia
Which observations provided the evidence for migration of the oceanic crust into the mantle:
Belts od volcanoes on continental margins
Discovery of the Benioff Zone
Identification of volcanic island arcs
Discovery of the Benioff Zone
The most characteristics feature of carbonate rocks in the Transvaal Supergroup are:
Stromatolites
Dolomites
Interbeds of Banded Iron Formations
Stromatolites
Dolomites
Interbeds of Banded Iron Formations
Sedimentation of the Transvaal Supergroup was terminated by the orogenesis:
Ubedian
Kheis
Kibara
Ubedian
In the Limpopo orogenic belt region, the following is/are exposed on the surface:
A set of nappes
The root zone of the orogen
Rocks of the continental crust
The root zone of the orogen
The age of the Uberian orogenic belt is:
1800Ma
1950Ma
2050Ma
1800Ma
The Waterberg Group contains rocks that are the oldest:
Red-beds
BIF
Gold-bearing strata
Red-beds
Amalgamation of the Rodinia Supercontinent is dated at:
2000Ma
1600Ma
1000Ma
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 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:
Archacan Basement rock
Pan-African island arc rock complexes
Mesoproterozoic Basement rocks
Archacan Basement rock
Pan-African island arc rock complexes
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 Taconian Orogenesis is:
Of the Ordovivian age
Resulted from diachronous collision
Resulted from collision continent-island arc
Of the Ordovivian age
Resulted from collision continent-island arc
The famous Castkill Delta originated:
Is a part of the Kaskaskia sequence
During the Arcadian orogenesis
During the Alleghenian orogenesis
Is a part of the Kaskaskia sequence
During the Arcadian orogenesis
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:
4
5
6
6
The Norilsk deposit is related to:
Postmagmatic fluids
Metamorphic remobilisation of the metals
Eruption of the Siberian Traps
Eruption of the Siberian Traps
The time when collision between India and Eurasia begun is:
45Ma
40Ma
55Ma
55Ma
The High Himalaya contain rocks:
Flysch with volcanic rocks
Related to the Tethys Ocean
The Gondwana formations
Related to the Tethys Ocean
In the zone of the Caledonian foldin in the NW Europe, the folds:
Extend NW-SE
Are genetically related to the collision between Baltica with Laurentia
Extend NE-SW
Are genetically related to the collision between Baltica with Laurentia

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