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WorksheetsGeochem and Geophysics
Total questions: 50
Worksheet time: 25mins
A correction for gravity variations with latitude due to Earth's oblate spheroid shape and the angular velocity decreasing from a maximum at the equator to zero at the poles
Drift Correction
Latitude Correction
Eotvos Correction
Elevation Correction
A survey type that is used mainly for the study of horizontal to near-horizontal interfaces where current and potential electrodes maintained at same relative spacing while whole spread is progressively expanded at a fixed point.
Electrical Resistivity
Induced Polarization
Electrical Profiling
Vertical Electrical Sounding (VES)
A method that measures the spatial variations in Earth's gravitational field strength. The operative physical property is Density
Gravity
Electrical
Self-Potential
Electromagnetic
It measures the travel times of reflected or refracted seismic waves using as operative properties the density and elastic moduli, which determine the propagation velocity of seismic waves.
Electrical
Induced Polarization
Seismic
Gravity
Corrects for the decrease in gravity with height in free air due to increased distance from the center of the Earth.
Gravity Reduction
Free-air Correction (FAC)
Drift Correction
Bouguer Correction
The magnetic equivalent of latitude correction in gravity surveying, this correction removes the effect of a geomagnetic reference field (regional field) from the data.
Tidal Correction
Bouguer Correction
Electromagnetic Correction
Geomagnetic Correction
Used to determine lateral variations of resistivity where current and potential electrodes maintained at fixed spacing and progressively moved along a profile.
Electrical Profiling
Electromagnetic Sounding
Vertical Electrical Sounding
Electrical Resistivity
The living evidence of isostasy with the removal of 2.5-km thick ice at the end of the last ice age 10,000 years ago. its current peak uplift rate is 9mm/yr and the remaining uplift is estimated to be about 75-110 km.
Slovakia
Fennoscandia
Scandinavia
Greenland
Refers to the difference in mass between the body and the mass of country rock that would otherwise fill the space occupied by the body
Excess Mass
Causative Body
Anomalous Body
Dilatency
A type of resistivity array that denotes constant separation between the electrodes and the distance between B and M can be increased to be an integral multiple (n) and (a).
Sonde Spread
Wenner Spread
Dipole-Dipole Spread
Schlumberger Spread
the logging method that measures the bulk apparent conductivity of the formation and pore-fluid surrounds the borehole.
Electromagnetic Induction
Caliper
Fluid Resistivity
Electromagnetic and Spinner Flowmeter
A logging method that measures the resistivity of formation with additional data, true resistivity and can be calculated.
Fluid Resistivity
Single-point reason
Acoustic Resistivity
Normal Resistivity
Which of the following are the appropriate survey methods for exploration of metalliferous mineral deposits?
Magnetics, Electromagnetics, Electrical Resistivity, Self-potential, Induced Polarization, Radiometric
Seismic, Gravity, Magnetics, Electromagnetics
Seismic, Electrical Resistivity, Gravity
Electrical Resistivity, Seismic, Ground Penetrating Radar, Gravity, Magnetics
A device for converting electrical energy into acoustic energy. Its pulse is generated by the discharge of a large capacitor bank directly into the sea water through an array of electrodes towed in a frame behind the survey vessels.
Boomers
Vibroseis
Sparkers
Airgun
A weighted average across n-layers that factors out the differences in travel time spent in layers of differing velocity.
Two-way travel time
Root-Mean-Square (RMS)
Normal moveout
Mean travel time
Where does wave reflection or refraction occur?
On the surface
At the interface between two materials if the wave changes velocity
Inside the material, if the wave changes its velocity
If the material has the same composition
What happens to wave velocities as they occur deeper in the mantle?
Their velocity increases
Their velocity decreases
Their velocity remains the same
It cannot penetrate
What is the P wave shadow zone?
The zone where the P waves duplicate, forming multiples
The zone where P waves and S waves cannot pass through
Band along the core where P waves cannot pass through
Band along the surface where P waves do not occur
An equipotential surface which coincides with the mean sea level on imaginary earth in which all masses are uniformly distributed laterally. This earth has the same total mass and size (volume) as the real earth
Root-Mean-Square Velocity (RMS)
Geoid
Reference ellipsoid (spheroid)
Terrain Correction
Waves along interface sends waves back to surface at critical angle. It can arrive before the direct waves- only happens past critical distance
Asymptotic Refraction
Reflected Ray
Non-vertical reflection
Critical Refraction
Which of the following would give a positive gravity anomaly?
Salt dome
Ore deposit
Spreading ridge
sediment filled garbon
Measures the time taken for a seismic wave to travel from a source (location known) into the ground where it is reflected back to the surface and detected by a receiver
Two-way travel time
Arrival time
Critical distance
Normal moveout
Which rock, mineral or ore has a resistivity of 100-5000 (ohm.m)?
Chalk
Quartzite
Sand
Gravel
Which rock, mineral or ore has a resistivity of 500-5000 (ohm.m)?
Sand
Sandstone
Limestone
Marl
How could you decrease resistivity?
decrease pore fluid, decrease salinity of pore fluid, add clay minerals, decrease permeability (connect pore, fracture rock)
Increase pore fluid, increase salinity of pore fluid, add clay minerals, increase permeability(connect pore, fracture rock)
decrease permeability(connect pore, fracture rock)
decrease pore fluid, increase salinity of pore fluid, add clay minerals, decrease permeability(connect pore, fracture rock)
A meteorite that has predominantly Ni-Fe alloys, minor amounts of other minerals such as troilite (FeS).
Achondrites
Stone Meteorites
Iron Meteorites
Stony-Iron Meteorites
This takes place when a minor element enters a crystal preferentially because it has a higher ionic potential than the ions of the major element (e.g., in the formation of feldspar crystals which may capture Ba2+ or Sr2+ in the place of K; as a result, the concentrations of these elements in the residual magma decrease during crystallization of K-feldspar)
Coupled Substitution
Adsorption
Capture
Admission
An alternative to coupled substitution in which ions are attached on the charged surfaces of small ions; usually displayed by the clay minerals.
Capture
Adsorption
Camouflage
Admission
Areas representing the range of applied pressure and temperature in which a mineral may exist in its stable form
Activation Energy
Phase Boundary
Thermodynamics
Stability Fields
A part or parts of a system occupying a specific volume and having uniform physical and chemical characteristics which distinguishes it from all other parts of the system.
Phase Boundary
Phase
Component
Phase Diagram
The point on a phase diagram where a reaction takes place between a previously precipitated phase and the liquid to produce a new solid phase. When this point is reached, the temperature must remain constant until the reaction has run to completion. Also an invariant point.
Eutectic point
Melting point
Peritectic point
Intermediate Point
At which the radioactive nuclide emits an electrons, thereby converting on of its neutron into a proton
Beta Decay
Alpha Decay
Lambda Decay
Gamma Decay
Measures the ability of an atom in a compound to attract electrons to itself. Metals have low (X) and noble gasses have a value of 0.Increases from left to right, and from bottom to top of the periodic table.
First Ionization Potential
Thermodynamics
Electronegativity
Electron configuration
Elements that are too large and or to highly charged to fit easily into common rock forming minerals that crystallize to form melts. (e.g., Large-ion Lithophile elements (LiL's) and "HFSE's")
Compatible elements
Major elements
Incompatible elements
Trace elements
Meteorites that is chiefly silicates, mostly ferromagnesian up t 1/4 metalli Ni-Fe types.
Iron meteorites
Stony-Iron meteorites
Chondrites
Stone meteorites
The diffusion rates of an element in and out of the crystal are unequal; there will be a net change of composition of each phase with me
Thermal Equilibrium
Disequilibrium
Equilibrium
Chemical equilibrium
Is the locus of temperatures (a curve on a phase diagram) below which a given substance is completely solid.
Liquidus
Eutectic point
Thermal Equilibrium
Solidus
Occurs when the minor element has the same charge and a similar ionic radius as the major element it is replacing.
Camouflage
Capture
Admission
Adsorption
These are all a wide range application of X-ray fluorescence, except?
Soil Survey
Research in igneous, sedimentary and metamorphic petrology
Petroleum Industry
identifying and charactersing the nature of clay minerals
An spectroanalytical procedure for the quantitative determination of chemical elements using the absorption of optical radiation (light) by free atoms in the gaseous state
Inductively Coupled Plasma Mass Spectrometry (ICP-MS)
X-ray fluorescence (XRF)
Atomic Absorption Spectroscopy (AAS)
X-ray diffraction (XRF)
Is the primary, non-destructive tool for identifying and quantifying the mineralogy of crystalline compounds in rocks, soils and particulates.
X-ray diffraction (XRD)
X-ray fluorescence (XRF)
Atomic Absorption Spectroscopy (AAS)
Electron microprobe (EDXA)
These are a very incompatible elements that do not substitute into major silicate phases (Although may replace Ti in titanite or rutile). High concentration of these imply an enriched source or extensive liquid evolution.
Zr, Hf
Nb, Ta
REE
Ni, Co, Cr
This element is commonly incompatible. Strongly partitioned into garnet and amphibole. Titanite and apatite also concentrate it, so the presence of these as accessories could have a significant effect.
Yttrium (Y)
Zirconium (Zr)
REE
Hafnium (Hf)
This trace element concentrates in pyroxenes and may be used as an indicator of pyroxene fractionation.
Cobalt (Co)
Zirconium (Zr)
Palladium (Pd)
Scandium (Sc)
Refractory residuum after basalt has been extracted by partial melting
Lherzolite
Dunite, Harzburgite
Sillimanite
Pyroxenite, Amphibolite
Fertile unaltered mantle
Lherzolite
Dunite
Harzburgite
Bridgmanite
Melting wherein a phase melts to a liquid with a composition different from the solid and produces a solid of different composition to the original solid.
Fractional melting
Batch Melting
Incongruent melting
Congruent melting
"Volatile elements", H, C, N, noble gases, occur in liquids or gases at temperatures and pressures found on or above the earth's surface
Lithophile elements
Atmophile elements
Chalcophile elements
Refractory elements
An open system process in which each increment of solid is immediately removed from the system as it forms.
Fractional Crystallization
Fractional Melting
Batch Melting
Assimilation
Separates the silica-saturated (sub-alkaline) from the silica undersaturated (alkaline) fields at low pressure.
Phase
Phase boundary
Thermal divide
Peritectic point
