Systematic heat flow measurements across the Wagner Basin, northern Gulf of California
A primary control on the geodynamics of rifting is the thermal regime. To better understand the geodynamics of rifting in the northern Gulf of California we systematically measured heat-flow across the Wagner Basin, a tectonically active basin that lies near the southern terminus of the Cerro Prieto...
|Published in:||Earth and planetary science letters, Vol. 479 (2017), p. 340-353|
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