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35:. Fissility is differentiated from scaly fabric in hand sample by the parting surfaces’ continuously parallel orientations to each other and to stratification. Fissility is distinguished from scaly fabric in thin section by the well-developed orientation of platy minerals such as
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during and after uplift. The effect of bioturbation has been documented well in shale cores sampled: past variable critical depths where burrowing organisms can no longer survive, shale fissility will become more pervasive and better defined.
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is the ability or tendency of a rock to split along flat planes of weakness (“parting surfaces”). These planes of weakness are oriented parallel to stratification in
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Fissility is used by some geologists as the defining characteristic which separates mudstone (no fissility) from shale (fissile). However, some professions, like
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and growth of micaceous minerals. A rock's fissility can be degraded in numerous ways during the geologic process, including clay particles
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Sedimentary
Petrology: An Introduction to the Origin of Sedimentary Rocks
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39:. Fissility is the result of sedimentary or metamorphic processes.
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Structural Fabric in Deep Sea
Drilling Project Cores from Forearcs
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78:, continue to use the terms shale and mudstone interchangeably.
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54:. Planes of weakness are developed in metamorphic rocks by the
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Planes of weakness are developed in sedimentary rocks such as
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Tendency of a rock to split along flat planes of weakness
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10.1130/0016-7606(1953)64[869:FOM]2.0.CO;2
120:Principles of North American Pre-Cambrian Geology
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140:. Geological Society of America. p. 24.
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117:Hise, Charles Richard Van (1896-01-01).
62:into a random fabric before compaction,
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516:List of tectonic plate interactions
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123:. U.S. Government Printing Office.
50:by clay particles aligning during
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161:Tucker, Maurice E. (2013-05-22).
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230:Sedimentology and Stratigraphy
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134:Moore, J. Casey (1986-01-01).
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110:
1:
188:Ingram, Roy L. (1953-08-01).
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973:. You can help Knowledge by
227:Nichols, Gary (2013-04-30).
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23:Slate displaying fissility
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601:Thick-skinned deformation
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233:. John Wiley & Sons.
167:. John Wiley & Sons.
1025:Structural geology stubs
606:Thin-skinned deformation
382:Stereographic projection
372:Orthographic projection
355:Measurement conventions
301:Lamé's stress ellipsoid
190:"Fissility of Mudrocks"
66:during compaction, and
24:
883:Paleostress inversion
576:Strike-slip tectonics
446:Extensional tectonics
426:Continental collision
296:Deformation mechanism
22:
461:Fold and thrust belt
965:This article about
893:Section restoration
769:Rock microstructure
431:Convergent boundary
331:Strain partitioning
316:Overburden pressure
306:Mohr–Coulomb theory
1020:Structural geology
967:structural geology
870:Kinematic analysis
526:Mountain formation
441:Divergent boundary
406:Accretionary wedge
282:Structural geology
98:Fracture (geology)
76:drilling engineers
25:
982:
981:
947:
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878:3D fold evolution
764:Pressure solution
759:Oblique foliation
639:Exfoliation joint
629:Columnar jointing
289:Underlying theory
147:978-0-8137-1166-9
56:recrystallization
33:sedimentary rocks
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682:Detachment fault
677:Cataclastic rock
611:Thrust tectonics
581:Structural basin
556:Pull-apart basin
496:Horst and graben
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88:Fabric (geology)
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817:Detachment fold
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717:Transform fault
692:Fault mechanics
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551:Plate tectonics
501:Intra-arc basin
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362:Brunton compass
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321:Rock mechanics
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200:(8): 869–878.
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174:978-1118698907
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311:Mohr's circle
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975:expanding it
964:
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707:Thrust fault
396:Large-scale
367:Inclinometer
341:Stress field
229:
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194:GSA Bulletin
193:
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129:
119:
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64:bioturbation
60:flocculating
41:
28:
27:In geology,
26:
888:Paleostress
774:Slickenside
749:Crenulation
702:Fault trace
697:Fault scarp
687:Disturbance
672:Cataclasite
561:Rift valley
481:Half-graben
451:Fault block
436:DĂ©collement
1014:Categories
916:Pure shear
903:Shear zone
860:Competence
744:Compaction
621:Fracturing
416:Autochthon
411:Allochthon
104:References
68:weathering
52:compaction
852:Boudinage
832:Monocline
827:Homocline
807:Anticline
789:Tectonite
779:Stylolite
754:Fissility
731:lineation
727:Foliation
591:Syneclise
536:Obduction
506:Inversion
398:tectonics
214:0016-7606
29:fissility
939:Category
911:Mylonite
842:Vergence
837:Syncline
739:Cleavage
664:Faulting
82:See also
48:mudstone
812:Chevron
799:Folding
644:Fissure
596:Terrane
541:Orogeny
521:MĂ©lange
456:Fenster
346:Tension
93:Fissure
586:Suture
571:Saddle
511:Klippe
476:Graben
336:Stress
326:Strain
237:
212:
171:
144:
969:is a
921:Shear
649:Joint
531:Nappe
491:Horst
486:Horse
44:shale
971:stub
822:Dome
729:and
654:Vein
634:Dike
566:Rift
377:Rake
235:ISBN
210:ISSN
169:ISBN
142:ISBN
37:mica
202:doi
46:or
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208:.
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.