Author: H.H. Rieke
Publisher: Elsevier
ISBN: 0080869270
Category : Science
Languages : en
Pages : 439
Book Description
Compaction of Argillaceous Sediments
Compaction of Argillaceous Sediments
Author: H.H. Rieke
Publisher: Elsevier
ISBN: 0080869270
Category : Science
Languages : en
Pages : 439
Book Description
Compaction of Argillaceous Sediments
Publisher: Elsevier
ISBN: 0080869270
Category : Science
Languages : en
Pages : 439
Book Description
Compaction of Argillaceous Sediments
Compaction of Argillaceous Sediments (20-500,000 Psi)
Author: Herman H. Rieke
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 1364
Book Description
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 1364
Book Description
Compaction of Coarse-Grained Sediments, I
Author: G.V. Chilingarian
Publisher: Elsevier
ISBN: 0080869297
Category : Technology & Engineering
Languages : en
Pages : 1365
Book Description
Compaction of Coarse-Grained Sediments, I
Publisher: Elsevier
ISBN: 0080869297
Category : Technology & Engineering
Languages : en
Pages : 1365
Book Description
Compaction of Coarse-Grained Sediments, I
Compaction and Development of Preferred Orietatin in Clayey Sediments
Author: Robert Heber Meade (Jr.)
Publisher:
ISBN:
Category :
Languages : en
Pages : 162
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 162
Book Description
Argillaceous Rock Atlas
Author: Neal R. O'Brien
Publisher: Springer Science & Business Media
ISBN: 1461234220
Category : Science
Languages : en
Pages : 322
Book Description
A major reason for the lack of understanding of argillaceous rocks is that the key to understanding their history lies in their microfabric. Argillaceous Rock Atlas addresses this aspect by taking a systematic approach to the analysis of shale fabrics. This approach combines such techniques as scanning electron microscopy, x-radiography and thin-section petrography. Thus the book is amply illustrated with scanning electron and thin section photomicrographs and x-radiograms which show the salient features of shale at a variety of scales. A great portion of the book is devoted to case studies, supplemented by mineralogical and geochemical data, which demonstrate the utility of these techniques in the interpretation of depositional environments, diagenetic processes and possible economic significance of argillaceous rocks. Argillaceous Rock Atlas is a valuable and unique reference for students and researchers involved in the fields of sedimentology and stratigraphy, petrology, petroleum geology, hydrogeology and geochemistry.
Publisher: Springer Science & Business Media
ISBN: 1461234220
Category : Science
Languages : en
Pages : 322
Book Description
A major reason for the lack of understanding of argillaceous rocks is that the key to understanding their history lies in their microfabric. Argillaceous Rock Atlas addresses this aspect by taking a systematic approach to the analysis of shale fabrics. This approach combines such techniques as scanning electron microscopy, x-radiography and thin-section petrography. Thus the book is amply illustrated with scanning electron and thin section photomicrographs and x-radiograms which show the salient features of shale at a variety of scales. A great portion of the book is devoted to case studies, supplemented by mineralogical and geochemical data, which demonstrate the utility of these techniques in the interpretation of depositional environments, diagenetic processes and possible economic significance of argillaceous rocks. Argillaceous Rock Atlas is a valuable and unique reference for students and researchers involved in the fields of sedimentology and stratigraphy, petrology, petroleum geology, hydrogeology and geochemistry.
Removal of Water and Rearrangement of Particles During the Compaction of Clayey Sediments
Author: Robert H. Meade
Publisher:
ISBN:
Category : Clay
Languages : en
Pages : 32
Book Description
Review of the pertinent literature on the factors influencing the water content and clay-particle fabric of clayey sediments under increasing overburden pressures.
Publisher:
ISBN:
Category : Clay
Languages : en
Pages : 32
Book Description
Review of the pertinent literature on the factors influencing the water content and clay-particle fabric of clayey sediments under increasing overburden pressures.
Sediment Compaction and Applications in Petroleum Geoscience
Author: Troyee Dasgupta
Publisher: Springer
ISBN: 3030134423
Category : Science
Languages : en
Pages : 119
Book Description
This book discusses how sediments compact with depth and applications of the compaction trends. Porosity reduction in sediment conveniently indicates the degree of sediments compacted after deposition. Published empirical curves- the compaction curves- are depth-wise porosity variation through which change in pore spaces from sediment surface to deeper depths e.g. up to 6 km can be delineated. Porosity is derived from well logs. Compaction curves, referred to as the Normal Porosity Profile of shales, sandstones and shale bearing sandstones of different models are reviewed along with the different mechanical and chemical compaction processes. These compaction models reveals how porosity reduces depth-wise and the probable reason for anomalous zones. Deviation from these normal compaction trends may indicate abnormal pressure scenarios: either over- or under pressure. We highlight global examples of abnormal pressure scenarios along with the different primary- and secondary mechanisms. Well logs and cores being the direct measurements of porosity, well log is the only cost-effective way to determine porosity of subsurface rocks. Certain well logs can detect overpressure and the preference of one log above the other helps reduce the uncertainty. Apart from delineation of under-compacted zones by comparing the modeled- with the actual compaction, porosity data can also estimate erosion.
Publisher: Springer
ISBN: 3030134423
Category : Science
Languages : en
Pages : 119
Book Description
This book discusses how sediments compact with depth and applications of the compaction trends. Porosity reduction in sediment conveniently indicates the degree of sediments compacted after deposition. Published empirical curves- the compaction curves- are depth-wise porosity variation through which change in pore spaces from sediment surface to deeper depths e.g. up to 6 km can be delineated. Porosity is derived from well logs. Compaction curves, referred to as the Normal Porosity Profile of shales, sandstones and shale bearing sandstones of different models are reviewed along with the different mechanical and chemical compaction processes. These compaction models reveals how porosity reduces depth-wise and the probable reason for anomalous zones. Deviation from these normal compaction trends may indicate abnormal pressure scenarios: either over- or under pressure. We highlight global examples of abnormal pressure scenarios along with the different primary- and secondary mechanisms. Well logs and cores being the direct measurements of porosity, well log is the only cost-effective way to determine porosity of subsurface rocks. Certain well logs can detect overpressure and the preference of one log above the other helps reduce the uncertainty. Apart from delineation of under-compacted zones by comparing the modeled- with the actual compaction, porosity data can also estimate erosion.
Geology of Argillaceous Sediments
Author: Paul Edwin Potter
Publisher:
ISBN:
Category : Sediments (Geology)
Languages : en
Pages : 144
Book Description
Publisher:
ISBN:
Category : Sediments (Geology)
Languages : en
Pages : 144
Book Description
The Petrology of the Sedimentary Rocks
Author: Frederick Henry Hatch
Publisher:
ISBN:
Category : Petrology
Languages : en
Pages : 454
Book Description
Publisher:
ISBN:
Category : Petrology
Languages : en
Pages : 454
Book Description
Geology Or [i.e. Of] Argillaceous Sediments
Author: Paul Edwin Potter
Publisher:
ISBN:
Category : Clay
Languages : en
Pages : 142
Book Description
Publisher:
ISBN:
Category : Clay
Languages : en
Pages : 142
Book Description