4th year geology students Of ore petrology and applied sedimentology

 

Final exam. Of ore petrology and applied sedimentology for 4th year geology students

First semester ( January 2011)                                                    Time allowed 2 hours

 

A- Applied sedimentology

 

Answer the following questions illustrating your word whenever possible:

1- The roll-front uranium ore is controlled by weathering process and environment of deposition, explain this and give an example from the geological record for this type of ore. (20 marks)

 

2- Tick the correct statement and put (x) by the false one: (15 marks)

      a- Cinnabar mineral is one of the most dangerous mineral.

      b- Eolian sand is suitable for making concrete.

      c- Placers can accumulate on the lee side of sand dunes.

      d- Granite wash serve as good oil reservoir.

      e- All porous rocks are permeable.

 

3- Complete the following sentences: (10 marks)

      a- Limestone is very important sedimentary rocks. Several important industries depend on it as 1- ………..,2-…………. 3-

      b- Fluvial deposits are very important because 1…………. 2———— 3——–

      c- Weathering products may be solids which remain in situ as residual deposits  as …………, ……….and …………….or go in solution as ………and ……..             

 

B- Ore Petrology

 

1- Explain briefly (with illustrations):

A) The petrological interrelationships of ore minerals in the following ore deposits: (15 marks)

1) Fe-Ti oxide deposits.

2) Fe- Cu-Ni sulfide deposits.

3) Alpine-type chromite deposits.

B) The method of Sharpe et al (1985) of arsenopyrite geothermometry. (5 marks)

 

2-Choose the correct answer (10 marks)

a- Growth of sulfide minerals in lavas takes place in the form of (skeletal crystals – round droplets – euhedral to subhedral crystals).

 

b- The tubular disconcordant orebodies are characterized by (pinch and swell structurebranching and  anastomosing stockworks).

 

c- (Stratiform – Starabound – Disseminated) deposits show a considerable development parallel to bedding and a limited development perpendicular to it.

 

d- Diamond deposits in kimberlite represent (concordant orebodies- discordant orebodies- residual orebodies).

 

e- Replacement of magnetite by martite is carried out through (change in oxidation state – change in anions – selective remove of one cation).

 

4- Put (Ö) after the true statement and (X) after the false one in the following: (10 marks)

A-Rounding-off of wall-rock surfaces on both sides of a mineral deposit within a fracture indicates its formation by open space deposition.                                                           (X).                                    

 

B- Starabound orebodies are restricted to a particular part of the stratigraphic column, regardless whether the orebody is concordant or discordant.                                      (Ö ).

  

C-“Pinch and swell structure” results from later replacement of fracture walls        (X).

 

D- Layered chromite deposits are formed in tectonically unstable environments while podiform ones are formed in tectonically stable conditions.                                             (X).

 

E- Metamorphic fluids are produced by break down of hydrous silicate and carbonate minerals at the transition from greenscist to amphipolite facies.                                     (Ö ).

 

5- Complete the missing parts in the following statements (5 marks):

A) Breccia ore results from deformation of crustified veins during or after ore formation.

B)- The exsolution type in which structures of both phases are completely different or without crystallographic continuity across the interface between phases is called incoherent exsolution.

C- Experimental work showed that chalcopyrite disease is not an exsolution, so it is most propably to be epitaxial growth or replacement by Cu-rich fluids (any or both).

DVMS deposits are generally stratiform lenticular or sheetlike orebodies developed at interfaces or horizons of pauses in volcanism or change from volcanism to sedimentation.

E- In Ag-Bi-Co-Ni-As vein deposits, native silver is petrologically found in dendritic  patterns that are surrounded by rosettes of colloform arsenides.

__________________________________________________________________________

 

        Good luck            __________________________ Dr. Abdel Aziz El Haddad

                                                                                                   Dr. Ahmed Abdelrasheed

4th year geology students Of ore petrology and applied sedimentology
تمرير للأعلى