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, 2011 Reefs have caused a tremendous interest in diagenetic studies in the past decades, with a particular exponential development during the 70’ and 80’, just after the major discovery of the early submarine cements in modern coral reef complexes in the late 60's (Ginsburg et al. 1967; Macintyre et al. 1968; Land and Goreau 1970; ...).
Perrin, Christine
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Diagenesis in Progress, Progress in Diagenesis – The Skeletal Archives [PDF]
Quaternary International, 2023 Skeletal remains serve as first-hand witnesses of our past, providing crucial information for reconstructing important events in human and animal history. These valuable remains hold information about the dietary habits, mobility patterns, biological profile and, genetic history of the individual during its life.
Maurer, Anne-France, Salesse, Kevin
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Diagenesis of archaeological bone and tooth [PDF]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2018 An understanding of the structural complexity of mineralised tissues is fundamental for exploration into the field of diagenesis. Here we review aspects of current and past research on bone and tooth diagenesis using the most comprehensive collection of ...
Anne Marie Høier Eriksen +2 more
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Quantifying early marine diagenesis in shallow-water carbonate sediments
Geochimica Et Cosmochimica Acta, 2018 Shallow-water carbonate sediments constitute one of the most abundant and widely used archives of Earth’s surface evolution. One of the main limitations of this archive is the susceptibility of the chemistry of carbonate sediments to post-depositional ...
Anne-Sofie C Ahm +2 more
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AAPG Bulletin, 1958
ABSTRACT Most sediments are mixtures of many heterogeneous compounds and are chemically unstable. Low temperature and pressure may permit a sediment to remain in metastable conditions for hundreds of millions of years, but normally changes occur, leading to the separation of different chemical compounds, with water and organic matter ...
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ABSTRACT Most sediments are mixtures of many heterogeneous compounds and are chemically unstable. Low temperature and pressure may permit a sediment to remain in metastable conditions for hundreds of millions of years, but normally changes occur, leading to the separation of different chemical compounds, with water and organic matter ...
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Journal of Geological Education, 1994
Simple models which allow fluids to percolate through sands of varying grain-size and porosity distribution provide a useful analog for students to view the regional geometry of diagenesis.
C.J.R. Braithwaite, Giancarlo Rizzi
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Simple models which allow fluids to percolate through sands of varying grain-size and porosity distribution provide a useful analog for students to view the regional geometry of diagenesis.
C.J.R. Braithwaite, Giancarlo Rizzi
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Diagenesis: general considerations
1982The transformation of a freshly deposited sediment into a rock is a complex process. Diagenesis is the name given to the many chemical and physical processes which act upon sediment grains in the subsurface. Halmyrolysis refers to the more restricted aspect of chemical changes operative at the sediment/water interface.
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