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Fissility (geology)

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20: 935: 959: 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 70:
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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Structural Fabric in Deep Sea Drilling Project Cores from Forearcs
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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 1011: 994: 266: 140:. Geological Society of America. p. 24. 1001: 987: 273: 259: 117:Hise, Charles Richard Van (1896-01-01). 62:into a random fabric before compaction, 18: 226: 1012: 280: 187: 160: 254: 133: 953: 116: 516:List of tectonic plate interactions 13: 123:. U.S. Government Printing Office. 50:by clay particles aligning during 14: 1036: 161:Tucker, Maurice E. (2013-05-22). 957: 934: 933: 230:Sedimentology and Stratigraphy 220: 181: 154: 134:Moore, J. Casey (1986-01-01). 127: 110: 1: 188:Ingram, Roy L. (1953-08-01). 103: 973:. You can help Knowledge by 227:Nichols, Gary (2013-04-30). 7: 81: 10: 1041: 952: 23:Slate displaying fissility 929: 901: 868: 850: 797: 725: 662: 619: 601:Thick-skinned deformation 395: 354: 288: 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:LamĂ©'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: 946: 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 1032: 1003: 996: 989: 961: 954: 937: 936: 682:Detachment fault 677:Cataclastic rock 611:Thrust tectonics 581:Structural basin 556:Pull-apart basin 496:Horst and graben 275: 268: 261: 252: 251: 245: 244: 224: 218: 217: 185: 179: 178: 158: 152: 151: 131: 125: 124: 114: 88:Fabric (geology) 1040: 1039: 1035: 1034: 1033: 1031: 1030: 1029: 1010: 1009: 1008: 1007: 950: 948: 943: 925: 897: 864: 846: 817:Detachment fold 793: 721: 717:Transform fault 692:Fault mechanics 658: 615: 551:Plate tectonics 501:Intra-arc basin 391: 362:Brunton compass 350: 284: 279: 249: 248: 241: 225: 221: 186: 182: 175: 159: 155: 148: 132: 128: 115: 111: 106: 84: 17: 12: 11: 5: 1038: 1028: 1027: 1022: 1006: 1005: 998: 991: 983: 980: 979: 962: 945: 944: 942: 941: 930: 927: 926: 924: 923: 918: 913: 907: 905: 899: 898: 896: 895: 890: 885: 880: 874: 872: 866: 865: 863: 862: 856: 854: 848: 847: 845: 844: 839: 834: 829: 824: 819: 814: 809: 803: 801: 795: 794: 792: 791: 786: 784:Tectonic phase 781: 776: 771: 766: 761: 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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 1016:: 208:. 198:64 196:. 192:. 1002:e 995:t 988:v 977:. 274:e 267:t 260:v 243:. 216:. 204:: 177:. 150:.

Index


sedimentary rocks
mica
shale
mudstone
compaction
recrystallization
flocculating
bioturbation
weathering
drilling engineers
Fabric (geology)
Fissure
Fracture (geology)
Principles of North American Pre-Cambrian Geology
Structural Fabric in Deep Sea Drilling Project Cores from Forearcs
ISBN
978-0-8137-1166-9
Sedimentary Petrology: An Introduction to the Origin of Sedimentary Rocks
ISBN
978-1118698907
"Fissility of Mudrocks"
doi
10.1130/0016-7606(1953)64[869:FOM]2.0.CO;2
ISSN
0016-7606
Sedimentology and Stratigraphy
ISBN
9781118687772
v

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