Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments

Diagenesis of carbonates and clastic sediments encompasses the biochemical, mechanical, and chemical changes that occur in sediments subsequent to deposition and prior to low-grade metamorphism. These parameters which, to a large extent, control diagenesis in carbonates and clastic sediments include...

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Udgivet: MDPI - Multidisciplinary Digital Publishing Institute 2022
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description Diagenesis of carbonates and clastic sediments encompasses the biochemical, mechanical, and chemical changes that occur in sediments subsequent to deposition and prior to low-grade metamorphism. These parameters which, to a large extent, control diagenesis in carbonates and clastic sediments include primary composition of the sediments, depositional facies, pore water chemistry, burial–thermal and tectonic evolution of the basin, and paleo-climatic conditions. Diagenetic processes involve widespread chemical, mineralogical, and isotopic modifications affected by the original mineralogy of carbonate and clastic sediments. These diagenetic alterations will impose a major control on porosity and permeability and hence on hydrocarbon reservoirs, water aquifers, and the presence of other important economic minerals. In this Special Issue, we have submissions focusing on understanding the interplay between the mineralogical and chemical changes in carbonates and clastic sediments and the diagenetic processes, fluid flow, tectonics, and mineral reactions at variable scales and environments from a verity of sedimentary basins. Quantitative analyses of diagenetic reactions in these sediments using a variety of techniques are essential for understanding the pathways of these reactions in different diagenetic environments.
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language eng
publishDate 2022
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publisher MDPI - Multidisciplinary Digital Publishing Institute
publisherStr MDPI - Multidisciplinary Digital Publishing Institute
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spelling doab-20.500.12854ir-764132024-03-27T16:34:43Z Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments Al-Aasm, Ihsan Mansurbeg, Howri diagenesis authigenic minerals reservoir quality Eboliang Qaidam Basin clay minerals major elements trace elements sedimentary environment diagenetic Environment silicification meteoric diagenesis fractures deltaic sequence karst glacial period dolomitization Huron Domain Silurian Devonian fluid composition Michigan Basin bipyramidal quartz pseudohexagonal aragonite Iberian Range Upper Triassic hydrothermal circulation carbonate reservoirs sedimentation porosity platform carbonates REE + Y chemistry paleoceanographic proxies diagenetic proxies NE Turkey hydrothermal dolomite diagenetic settings optical petrography geochemical Triassic-Jurassic successions Provençal Domain n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general Diagenesis of carbonates and clastic sediments encompasses the biochemical, mechanical, and chemical changes that occur in sediments subsequent to deposition and prior to low-grade metamorphism. These parameters which, to a large extent, control diagenesis in carbonates and clastic sediments include primary composition of the sediments, depositional facies, pore water chemistry, burial–thermal and tectonic evolution of the basin, and paleo-climatic conditions. Diagenetic processes involve widespread chemical, mineralogical, and isotopic modifications affected by the original mineralogy of carbonate and clastic sediments. These diagenetic alterations will impose a major control on porosity and permeability and hence on hydrocarbon reservoirs, water aquifers, and the presence of other important economic minerals. In this Special Issue, we have submissions focusing on understanding the interplay between the mineralogical and chemical changes in carbonates and clastic sediments and the diagenetic processes, fluid flow, tectonics, and mineral reactions at variable scales and environments from a verity of sedimentary basins. Quantitative analyses of diagenetic reactions in these sediments using a variety of techniques are essential for understanding the pathways of these reactions in different diagenetic environments. 2022-01-11T13:31:15Z 2022-01-11T13:31:15Z 2021 book ONIX_20220111_9783036500782_149 9783036500782 9783036500799 https://directory.doabooks.org/handle/20.500.12854/76413 eng image/jpeg Attribution 4.0 International https://mdpi.com/books/pdfview/book/3848 https://mdpi.com/books/pdfview/book/3848 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-0365-0079-9 10.3390/books978-3-0365-0079-9 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783036500782 9783036500799 218 Basel, Switzerland open access
spellingShingle diagenesis
authigenic minerals
reservoir quality
Eboliang
Qaidam Basin
clay minerals
major elements
trace elements
sedimentary environment
diagenetic Environment
silicification
meteoric diagenesis
fractures
deltaic sequence
karst
glacial period
dolomitization
Huron Domain
Silurian
Devonian
fluid composition
Michigan Basin
bipyramidal quartz
pseudohexagonal aragonite
Iberian Range
Upper Triassic
hydrothermal circulation
carbonate reservoirs
sedimentation
porosity
platform carbonates
REE + Y chemistry
paleoceanographic proxies
diagenetic proxies
NE Turkey
hydrothermal dolomite
diagenetic settings
optical petrography
geochemical
Triassic-Jurassic successions
Provençal Domain
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title_full Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title_fullStr Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title_full_unstemmed Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title_short Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
title_sort chemical mineralogical and isotopic studies of diagenesis of carbonate and clastic sediments
topic diagenesis
authigenic minerals
reservoir quality
Eboliang
Qaidam Basin
clay minerals
major elements
trace elements
sedimentary environment
diagenetic Environment
silicification
meteoric diagenesis
fractures
deltaic sequence
karst
glacial period
dolomitization
Huron Domain
Silurian
Devonian
fluid composition
Michigan Basin
bipyramidal quartz
pseudohexagonal aragonite
Iberian Range
Upper Triassic
hydrothermal circulation
carbonate reservoirs
sedimentation
porosity
platform carbonates
REE + Y chemistry
paleoceanographic proxies
diagenetic proxies
NE Turkey
hydrothermal dolomite
diagenetic settings
optical petrography
geochemical
Triassic-Jurassic successions
Provençal Domain
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
topic_facet diagenesis
authigenic minerals
reservoir quality
Eboliang
Qaidam Basin
clay minerals
major elements
trace elements
sedimentary environment
diagenetic Environment
silicification
meteoric diagenesis
fractures
deltaic sequence
karst
glacial period
dolomitization
Huron Domain
Silurian
Devonian
fluid composition
Michigan Basin
bipyramidal quartz
pseudohexagonal aragonite
Iberian Range
Upper Triassic
hydrothermal circulation
carbonate reservoirs
sedimentation
porosity
platform carbonates
REE + Y chemistry
paleoceanographic proxies
diagenetic proxies
NE Turkey
hydrothermal dolomite
diagenetic settings
optical petrography
geochemical
Triassic-Jurassic successions
Provençal Domain
n/a
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
url ONIX_20220111_9783036500782_149