Robert Ondrak scite author profile

The Cameros Basin (North Spain) is a Late Jurassic-Early Cretaceous extensional basin, which was inverted during the Cenozoic. It underwent a remarkable thermal evolution, as indicated by the record of anomalous high temperatures in its deposits. In this work the subsidence and thermal history of the basin is reconstructed, using subsidence analysis and 2D thermal modeling. Accepted ArticleThis article is protected by copyright. All rights reserved.

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A three-dimensional insight into the Mackenzie Basin (Canada): Implications for the thermal history and hydrocarbon generation potential of Tertiary deltaic sequences

Kroeger

Ondrak

Primio

et al. 2008

Bulletin

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Quantifying erosion rates in the Molasse basin using a high resolution data set and a new thermal model

Hagke¹,

Lujiendjik²,

Ondrak³

et al. 2015

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Robert Ondrak

Living microbial ecosystems within the active zone of catagenesis: Implications for feeding the deep biosphere

Deep basin gas: New insights from kinetic modelling and isotopic fractionation in deep-formed gas precursors

Subsidence and thermal history of an inverted Late Jurassic‐Early Cretaceous extensional basin (Cameros, North‐central Spain) affected by very low‐ to low‐grade metamorphism

A three-dimensional insight into the Mackenzie Basin (Canada): Implications for the thermal history and hydrocarbon generation potential of Tertiary deltaic sequences

Quantifying erosion rates in the Molasse basin using a high resolution data set and a new thermal model

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