4 structural geology

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    Introduction to oil feld

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    STRUCTURAL GEOLOGY

    Structural Geology is study o change in rockstructure !eor"ation# due internal$e%ternalorces such as stress and strain&

    These orces a''lied due to tectonic acti(ities oearth&

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    )ASIC TER*I+OLOGY

    Strike and di' reer to the orientation orattitude o a geological eature&

    The strike line o a -ed. ault. or other 'lanar

    eature. is a line re'resenting the intersection othat eature /ith a hori0ontal 'lane&

    The di' gi(es the stee'est angle o descent o atilted -ed or eature relati(e to a hori0ontal'lane. and is gi(en -y the nu"-er 123412# as/ell as a letter +.S.E.5# /ith rough direction in

    /hich the -ed is di''ing&

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    TECTO+IC 6ORCES A+! ROC7)E8A9IER

    Rocks -eha(ior during tectonic orce is easilyunderstand -y Stress:strain cur(es and itsde'ends u'on the te"'erature o the Rock.

    direction o orce. ti"ing and the s'eed o theorces a''lied on it&

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    GEOLOGICAL 6EATURE

    Tectonic collision deor"s crustal rocks'roducing geologic structures&

    6olds

    6aults

    ;oints and 6ractures

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    6OL!

    Rocks are -ent -y crustal deor"ation into aseries o /a(e3like undulations called olds&

    *ost olds result ro" co"'ression stresses

    /hich shorten and thicken the crust&

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    Anticlines and Synclines are co""onin old and thrust -elts related to

    "ountain -elts

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    6igure

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    6AULT

    6aults are -reaks in rock units /ere "o(e"enthas occurred& There are three "a

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    continued

    ># Re(erse : 8anging /all "o(es u' relati(e tothe oot/all. caused -y co"'ressionshortening#&

    Re(erse aults ha(e di's greater than ?@ !egreeand thrust aults ha(e di's less then ?@ !egree&

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    Continued

    # Strike3Sli' : *o(e"ent along the ault ishori0ontal. 'arallel to the strike o the ault 'lane&I. standing on one side o the ault. the -lock on

    the other side is dis'laced to the right. the ault ister"ed right3lateral& I the -lock on the other sideis dis'laced to the let. the ault is ter"ed letlateral.

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    ;OI+TS

    They are ractures /ith no oBset&

    ;oints nor"ally ha(e a regular s'acing related toeither the "echanical 'ro'erties o the

    indi(idual rock or the thickness o the layerin(ol(ed

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