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CSIR-NET DEC 2018

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csir net(dec)-2018

107) A 2.0 km thick elevated land mass of density 2.7g/cc is associated with a Bouger anomaly of -176g/cc. The free air anamoly is (assume that 2πG = 42 mgals/km/g/cc). 

a) -51 mgals 
b)50 mgals
c) -85 mgals 
d) 85 mgals

(Thanks to Suresh Sir ANU)
(Thanks to Neeraja AU)

Sol:

\triangle g_B=g_m+(\triangle g_{FA}-\triangle g_{BP}+\triangle g_T+\triangle g_{tide})-g_n-(1)

\triangle g_F=g_m+(\triangle g_{FA}+\triangle g_T+\triangle g_{tide})-g_n-(2)

 Bouger anamoly (\triangle g_B) - Free  air anamoly(\triangle g_F) =-\triangle g_{BP}

\triangle g_B-\triangle g_F=-\triangle g_{BP}-(3a)

\triangle g_{BP}\rightarrow Bouger plate correction

\triangle g_{BP}=2\pi G\triangle\rho t-(4)

\triangle g_B-\triangle g_F=-2\pi G\triangle\rho t-(5)

\triangle\rho=2.7g/cc

\triangle g_B=-176mgals

2\pi G=42mgal/km/g/cc

\triangle g_B-\triangle g_F=-2\pi G\triangle\rho t-(5)

-176-\triangle g_F=-42\times2.7\times2

-176-\triangle g_F=-226.8

\triangle g_F=-226.8+176

-\triangle g_F=-50.8

\therefore \triangle g_F=50mgal

\therefore  Free air anamoly( \triangle g_F)=50mgal

g_m\rightarrow   measured  gravity  value

g_n\rightarrow normal  gravity  value

g_{FA}\rightarrow   Free air  correction

g_{BP}\rightarrow  Bouger  plate  correction

g_T\rightarrow   terrain  correction

g_{tide}{\rightarrow   tidal  correction}


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1 comment

  1. 1 km thick elevated landmass of density 2.7 gm/cc is associated with a free air anomaly that is half of bouger anomaly. If the density contrast at the mantle-crust boundary is 0.3 gm/cc, what would be the thickness of the root?
    1. 12 km
    2. 18 km
    3. 22.5 km
    4. 27 km

    ReplyDelete

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