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The Resource Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan, by Mehmet Koray Ekinci

Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan, by Mehmet Koray Ekinci

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Author
Contributor
Summary
The Nankai Trough, a convergent plate boundary between the subducting Philippine Sea plate and overriding Eurasian plate, is located off the coast of southwest Japan. This study covers the central portion of the Kumano transect, eastern province of the Nankai Trough, which consists of six morphotectonic zones, such as, from southeast to northwest, subduction inputs in the Shikoku Basin, trench zone, frontal thrust zone, imbricated thrust zone, megasplay fault zone, and Kumano forearc basin. The objectives of this study are: (1) to show how permeability varies as a function of burial depth, lithostratigraphy, and structural position within the Nankai Trough subduction zone; and (2) to document the permeability anisotropy and consider how it changes with microfabric and mineralogy. Constant-flow permeability tests were executed to measure permeability for vertical (along-core) and horizontal (cross-core) sections of twenty-one core samples collected during Integrated Ocean Drilling Program (IODP) Expeditions 316 and 333. Comparison of the horizontal (kh) to the vertical (kv) permeability defines the anisotropy (kh/kv). Environmental scanning electron microscopy (ESEM) was used to image the fabric of samples in horizontal and vertical sections. The images were analyzed to compute the standard deviations and the indexes (i) of microfabric orientation. The relative clay mineral percentages in bulk sediment were calculated using previously analyzed X-ray diffraction data
Language
eng
Work
Publication
Extent
1 online resource (xi, 143 pages)
Note
Advisor: Michael B. Underwood
Instance
Label
Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan
Title
Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan
Statement of responsibility
by Mehmet Koray Ekinci
Creator
Contributor
Author
Thesis advisor
Subject
Genre
Language
eng
Summary
The Nankai Trough, a convergent plate boundary between the subducting Philippine Sea plate and overriding Eurasian plate, is located off the coast of southwest Japan. This study covers the central portion of the Kumano transect, eastern province of the Nankai Trough, which consists of six morphotectonic zones, such as, from southeast to northwest, subduction inputs in the Shikoku Basin, trench zone, frontal thrust zone, imbricated thrust zone, megasplay fault zone, and Kumano forearc basin. The objectives of this study are: (1) to show how permeability varies as a function of burial depth, lithostratigraphy, and structural position within the Nankai Trough subduction zone; and (2) to document the permeability anisotropy and consider how it changes with microfabric and mineralogy. Constant-flow permeability tests were executed to measure permeability for vertical (along-core) and horizontal (cross-core) sections of twenty-one core samples collected during Integrated Ocean Drilling Program (IODP) Expeditions 316 and 333. Comparison of the horizontal (kh) to the vertical (kv) permeability defines the anisotropy (kh/kv). Environmental scanning electron microscopy (ESEM) was used to image the fabric of samples in horizontal and vertical sections. The images were analyzed to compute the standard deviations and the indexes (i) of microfabric orientation. The relative clay mineral percentages in bulk sediment were calculated using previously analyzed X-ray diffraction data
Cataloging source
MUU
http://library.link/vocab/creatorName
Ekinci, Mehmet Koray
Degree
M.S.
Dissertation note
Thesis
Dissertation year
2012.
Government publication
government publication of a state province territory dependency etc
Granting institution
University of Missouri--Columbia,
Index
no index present
Literary form
non fiction
Nature of contents
  • dictionaries
  • bibliography
  • theses
http://library.link/vocab/relatedWorkOrContributorName
Underwood, Michael B.
http://library.link/vocab/subjectName
  • Integrated Ocean Drilling Program
  • Clay minerals
  • Sediments (Geology)
  • Pacific Ocean
  • Japan
  • Morphotectonics
  • Scanning electron microscopy
  • X-rays
  • Anisotropy
  • Mineralogy
Label
Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan, by Mehmet Koray Ekinci
Instantiates
Publication
Note
Advisor: Michael B. Underwood
Carrier category
online resource
Carrier category code
  • cr
Carrier MARC source
rdacarrier
Content category
text
Content type code
  • txt
Content type MARC source
rdacontent
Control code
876615173
Extent
1 online resource (xi, 143 pages)
Form of item
online
Media category
computer
Media MARC source
rdamedia
Media type code
  • c
Other physical details
illustrations (some color)
Specific material designation
remote
System control number
(OCoLC)876615173
Label
Permeability, clay mineralogy, and microfabric of fine-grained sediments from the Nankai Trough and Shikoku Basin, offshore southwest Japan, by Mehmet Koray Ekinci
Publication
Note
Advisor: Michael B. Underwood
Carrier category
online resource
Carrier category code
  • cr
Carrier MARC source
rdacarrier
Content category
text
Content type code
  • txt
Content type MARC source
rdacontent
Control code
876615173
Extent
1 online resource (xi, 143 pages)
Form of item
online
Media category
computer
Media MARC source
rdamedia
Media type code
  • c
Other physical details
illustrations (some color)
Specific material designation
remote
System control number
(OCoLC)876615173

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