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- Volume 2, Issue 4, 1984
First Break - Volume 2, Issue 4, 1984
Volume 2, Issue 4, 1984
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Formation of rifted continental margins: a discussion of mechanisms
More LessSince the inception of plate teetonic concepts in the mid-1960s, the importance of thermal processes in the formation of rifted continent al margins has gradually been realised. It is now generally accepted that continental margin sediments are exposed to a decreasing geothermal gradient with time after continental breakup.
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Extraction of signatures from seismic and well data
Authors V. Danielsen and T.V. KarlssonTrace inversion is a weIl-known seismic method for deriving pseudo-acoustic impedance sections (Lindseth 1972). Prior to inversion a deconvolution of the seismic data is necessary to produce a pseudo-reflectivity section. Hence, the success of the inversion method depends on the stability of the seismic signature. One way of estimating the seismic pulse is to deconvolve the seismic traces with the weIl log reflectivity series.
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Volumes & issues
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Volume 42 (2024)
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Volume 41 (2023)
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Volume 40 (2022)
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Volume 39 (2021)
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Volume 38 (2020)
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Volume 37 (2019)
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Volume 36 (2018)
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Volume 35 (2017)
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Volume 34 (2016)
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Volume 33 (2015)
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Volume 32 (2014)
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Volume 31 (2013)
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Volume 30 (2012)
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Volume 29 (2011)
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Volume 27 (2009)
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Volume 25 (2007)
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Volume 24 (2006)
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Volume 23 (2005)
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Volume 22 (2004)
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Volume 21 (2003)
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Volume 20 (2002)
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Volume 19 (2001)
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Volume 18 (2000)
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Volume 17 (1999)
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Volume 16 (1998)
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Volume 15 (1997)
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Volume 14 (1996)
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Volume 13 (1995)
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Volume 12 (1994)
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Volume 11 (1993)
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Volume 10 (1992)
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Volume 9 (1991)
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Volume 8 (1990)
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Volume 7 (1989)
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Volume 6 (1988)
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Volume 5 (1987)
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Volume 4 (1986)
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Volume 3 (1985)
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Volume 2 (1984)
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Volume 1 (1983)