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Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

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Page 1: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Bernard BrunhesDiscovered rocks in France in 1906 with reversed magnetic polarity

Page 2: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 3: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Cretaceous ‘superchron’

Page 4: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Pacific Antarctic ridge

Schematic model

Page 5: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Drummond Matthews (left) and Fred VineCambridge University

Page 6: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Magnetic anomaliesover the ReykjanesRidge (S. of Iceland) from Vine & Matthews(1963).

Positive anomalies arecolored, negative onesare white.

Page 7: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Magnetic anomalypatterns acquired by the oceanic crust, while it formed during the Gilbert Reversed Chron (top) and afterwards (fromVine & Matthews,1963)

Gauss

Matuyama

Brunhes (today)

Gilbert

Page 8: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Juan de Fuca East Pacific Rise

observed

mirror image

model

Page 9: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Relative spreading rates

Page 10: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Blanco fracture zone

Page 11: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Alfred Wegener

Page 12: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Wegener’s map(1910). Note the distortion of India.

Map made witha computer(1965).

Page 13: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 14: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 15: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 16: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 17: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

The meaning of an “apparent” polarwander path (APWP).

Page 18: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 19: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

S. Keith Runcorn(1922 – 1995)

Page 20: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Computer-generatedfit of the Atlantic-bordering continents(Bullard et al., 1965),minimizing gaps and overlaps.

Page 21: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Ages of the Ocean floor determined from magnetic anomalies (~ 1990)

Page 22: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Late Cretaceous (~85 Ma) map of the world (Scotese, 1981)

www.scotese.com

Page 23: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Magnetic field during reversals

Page 24: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Geodynamo simulations (Glatzmaier and Roberts, 1996)

Inner core

Outer core

High fluid velocity intangent cylinder

Page 25: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity

Magnetic field lines

Close up of inner core

Page 26: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 27: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 28: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
Page 29: Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity