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

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Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity
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Transcript of Bernard Brunhes Discovered rocks in France in 1906 with reversed magnetic polarity.

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

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Cretaceous ‘superchron’

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Pacific Antarctic ridge

Schematic model

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Drummond Matthews (left) and Fred VineCambridge University

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

Positive anomalies arecolored, negative onesare white.

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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

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Juan de Fuca East Pacific Rise

observed

mirror image

model

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Relative spreading rates

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Blanco fracture zone

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Alfred Wegener

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

Map made witha computer(1965).

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

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S. Keith Runcorn(1922 – 1995)

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

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

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

www.scotese.com

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Magnetic field during reversals

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Geodynamo simulations (Glatzmaier and Roberts, 1996)

Inner core

Outer core

High fluid velocity intangent cylinder

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Magnetic field lines

Close up of inner core

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