Complementary Basin and Margin Thermal Evolution from Fission-Track

M. Rohrman; P. Andriessen; P. Van Der Beek

doi:10.3997/2214-4609.201409583

f Complementary Basin and Margin Thermal Evolution from Fission-Track
By M. Rohrman, P. Andriessen and P. Van Der Beek
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 57th EAGE Conference and Exhibition, May 1995, cp-90-00390
ISBN: 978-90-73781-06-1
DOI: https://doi.org/10.3997/2214-4609.201409583

Abstract

The thermal evolution of sedimentary basins and their margins is of major importance for hydrocarbon exploration as it controls the timing of hydrocarbon generation. During the last decade, apatite fission-track (AFT) thermochronology has become established as an important tool for unraveling thermal history information in the ~70° to 120°C temperature interval.

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1995-05-29

2024-04-24

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f Complementary Basin and Margin Thermal Evolution from Fission-Track

Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture