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Fig. 2.30 A pre-rift fit of Pangaea, based on Schettino
and Scotese ( 2005 ) and Schettino and Turco ( 2009 ). The
present day coastlines are shown for reference. The major
tectonic elements in this reconstruction are: central Africa
( CAF ), northwest Africa ( NWA ), northeast Africa ( NEA ),
Nubia ( NUB ), Somalia ( SOM ), Madagascar ( MAD ), Mo-
rocco ( MOR ), Arabia ( ARB ), India ( IND ), E. Antarctica
( EAN ), Australia ( AUS ), W. Antarctica ( WAN ), Brazilian
Craton ( BRA ), Paraná ( PA R ), Salado Block ( SAL ), Patag-
onia ( PAT ), N. America ( NAM ), Greenland ( GRN ), North
Slope ( NSL ), Okhotsk ( OKH ), Eurasia ( EUR ), Iberia
( IBE ), Amurian Plate ( AMU ), N. China ( NCH ), Yang Tze
Platform ( YTP ), and Indochina ( ICH )
Fig. 2.31 Geometrical fit
of conjugate COBs. In a
reference frame ( x 0 , y 0 , z 0 )
where a test Euler pole, e ,
hasbeenmovedtothe
North Pole, the fitting
procedure consists to find
the best rotation about the
North Pole, by an angle
that minimizes the squared
sum of longitude misfits
¥ i ( i
N )and• ¥ j ( j
M )
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