THE PRACTICE TEST
Practice test at a glance
- Questions
- 71
- Format
- Multiple choice
- Access
- 2 years
- Price
- $9.99
- Answers
- Included
- Explanations
- Included
GET FULL ACCESS
Unlock the full practice test
ONLINE ACCESS
$9.99
Unlock all 71 practice questions, answers and explanations.
- Immediate access after payment
- One question at a time in practice mode
- Jump directly to any question
- One-time payment
We'll send your purchase information to this address.
Payment is processed by PayPal.
TRY IT FIRST
Sample practice questions
Try some of the questions before buying. Answers and explanations are available with online access.
Sodic series is a subgroup of alkaline series Tholeiitic series is a subgroup of subalkaline series Potassic series is a subgroup of alkaline series Calk-alkaline series is a subgroup of alkaline series
Na Ca Fe Mg
Alkaline basalts and basanites are primitive because they have restite-rich nodules Tholeiitic basalts are primitive because they have restite-rich nodules Tholeiitic basalts are primitive because they don't have restite-rich nodules Calc-alkaline basalts are primitive because they have restite-rich nodules
Fast-spreading ridges have broader range of compositions and a larger proportion of evolved liquids Slow-spreading ridges have broader range of compositions Composition of MORB in both fast and slow-spreading ridges are the same MORB is completely uniform magmas
Archaen Precambrian Jurassic Eocene
hybrid of N-MORB and OIB OIT OIA hybrid of E-MORB and OIB
peralkaline calc-alkaline aluminous sodic
it is denser magma has more Mg Mg is smaller than Fe Fe is used by pyroxene and magnettite
Alkaline Tholeiitic Calc-alkaline Alkaline and tholeiitic
subduction zones oceanic rifts continental rifts hot spots
SiO2, H2O content MgO and volatiles Fe, Si and volatiles Evolution trend
The presence of water in calc-alkaline/absence of water in tholeiite Higher SiO2 in C.a Lower K2O in T Higher incompatible elements in C.a
I-type S-type Hybrid Plagiogranites
LMI, LMI LMI, continental rift intrusion continental rift intrusion, LMI both hot spot related intrusions
siderophile, chalcophile chalcophile, siderophile chalcophile, chalcophile lithophile, chalcophile
high, high if the melting materials are mafic high, low low, low if the melting materials are mafic low, high
basalt, andesite andesite, rhyolite andesite, rhyodacite, rhyolite basalt, andesite, rhyolite
That element will partition toward solid phase That element will partition toward liquid phase That element will not partition between liquid and solid phases That element would partition toward solid only in the early stage of crystallization
metaluminous peralkaline peraluminous peralkaline and peraluminous
ocean-ocean, ocean-continent subduction ocean-ocean, ocean-ocean subduction ocean-continent, ocean-ocean subduction ocean-ocean, continent-continent subduction
oceanic because specific gravity of oceanic crust is high continental because specific gravity of oceanic crust is low continental because specific gravity of oceanic crust is high oceanic because oceanic crust is thinner
Tholeiitic Calk-Alkaline Both above Alkaline
Opx Cpx Plag Olivine
To reduce the high values of some REE's To increase the proportions of some REE's To eliminate Oddo-Harkins effect To produce a smooth pattern
alkaline tholeiitic calc-alkaline both alkaline and tholeiitic
That element will partition toward solid phase That element will partition toward liquid phase That element will not partition between liquid and solid phases That element would partition toward solid only in the early stage of crystallization
benmorite ankaramite charnockite mugearite
Qtz Olivine Opx
Magma originated from the mantle Magma assimilated some crustal rocks during ascent Plag fractionated from the magma Eu was low in the source
fO2 pH T P
Alkaline basalt Tholeiitic basalt Calc-alkaline basalt Alkaline and tholeiitic basalt
Basaltic andesite Andesite Dacite Rhyolite
200 km 50 km 110 km 350 km
alkaline calc-alkaline aluminous peralkaline
V Ti Na HREE
forearc back-arc volcanic front volcanic arc
Ni V Ti Na
That element will partition toward solid phase That element will partition toward liquid phase That element will not partition between liquid and solid phases That element would partition toward solid only in the early stage of crystallization
Hot spots occur only in oceanic crust Volcanic hot spots create linear chains The source of magma in hot spots is the mantle Both alkaline and tholeiitic basalts are formed in hot spots
OIB MORB Calc-alkaline andesite in subduction zones Alkaline and tholeiitic basalt formed in continental rifts
ocean-ocean subduction zones oceanic rifts continental rifts hot spots
oceanic rifts continental rifts hot spots any tectonic setting
Depleted mantle Enriched mantle Mixing of N-MORB and E-MORB magmas Mixing of enriched mantle magma with tonalitic basalt
Sm, LREE HREE, Eu HREE, LREE Eu, HREE
minima moves towards Ab-Or side ... towards Ab-Qtz side ... towards Qtz-Or side
alkaline tholeiitic calc-alkaline mixed
They can be olivine-bearing They can be quartz-bearing They can be olivine-bearing or quartz-bearing, depending on which side of the plane of silica saturation they plot They cannot be quartz bearing
La/Sm, Tb/Lu Tb/Lu, La/Sm La/Eu, Sm/Lu Sm/La, Eu/Lu
Thickening of the crust Thermal disturbance Mantle effects All above
Opx Cpx Plag Olivine
Al2O3 Al2O3>CaO+Na2O+K2O Al2O3Na2O+K2O
There is no basalt associated with stratovolcanoes Basalts are widespread but do not commonly erupt from stratos Pyroclastic materials are less common in stratos Stratos usually consist of predominantly dacitic lava
supplying heat supplying material supplying heat and/or material
alkaline calc-alkaline aluminous peralkaline
convergent margin mid-ocean rift intraplate setting continental rift
Depleted mantle Enriched mantle Ancient oceanic crust or sediments Assimilation of continental crust
subsolvus granites hypersolvus granites alkaline granites calc-alkaline granites
Plag CPX OPX Either plag or cpx depending on the magma series
subsolvus granites hypersolvus granites alkaline granites calc-alkaline granites
OH Ni Ta Ti
Calc-alkaline trend Tholeiitic trend Alkaline trend Both calk-alkaline and tholeiitic trends
Lu La Sm Eu
corroded/embayed margins corona oscillatory zoning all of them
All alkaline rocks show the same evolution trend All subalkaline rocks show the same evolution trend
subduction zones oceanic rifts continental rifts hot spots
Jurassic Eocene Cretaceous Archaen
Alkaline, tholeiitic Tholeiitic, alkaline Calc-alkaline, tholeiitic Alkaline, calc-alkaline
Magma originated from the crustal source Magma assimilated some crustal rocks during ascent Eu was high in the source The was plag in the source
Volcanism is uniformly developed in island arc Volcanism is continuous along island arc axis Both compression and extension happen in a subduction zone Thickness of the continental crust remains unchanged during subduction
CS/CL CL/CS CS/CS CL/CL
subduction zones oceanic rifts continental rifts hot spots
Ready for all 71 questions?
Unlock the full practice test