Knowledge (XXG)

Piggyback basin

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or syndepositional growth structures. The piggyback basin is named after its tendency to be carried passively toward the hinterland with the old thrust sheet in response to the compressive forces of the new thrust sheet. Sedimentary fill for the basin come from the
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Wagreich M., A slope-apron succession filling a piggyback basin: the Tannheim and Losenstein Formations (Aptian - Cenomanian) of the eastern part of the Northern Calcareous Alps (Austria), Universuty of Vienna, 2003
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or from the sides of the basin. Drainage into the basin may come from highs associated with the thrust sheets or the basin may be filled from longitudinal flows across the basin.
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have small sedimentary basins which were example basins used to initially describe the occurrence and tectonics of piggyback basins. The Tannheim-Losenstein basin in the
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system. Piggyback basins form in the wedge-top depositional zone of a foreland basin system as new thrusts in the foreland cut up through the existing
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Allen, Philip A. and Allen, John R. (2005) Basin Analysis: Principles and Applications, 2nd ed., Blackwell Publishing, 549 pp.
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Ori, Gian Gabriele; Friend, Peter (1994). "Sedimentary basins formed and carried piggy-back on active thrust sheets".
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containing the eroded wedge-top basins in the old thrust sheet. The basin is separated from the foredeep by an
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10.1130/0091-7613(1984)12<475:sbfacp>2.0.co;2
197: 61:ramp of the older thrust sheet, from the foreland 217: 8: 224: 210: 76:and the Pyrenean (northern) margin of the 100: – Foreland basin north of the Alps 110: 68:The Apennine (southern) margin of the 7: 178: 176: 196:. You can help Knowledge (XXG) by 88:is a deep marine piggyback basin. 14: 180: 1: 159:Encyclopedia of Geomorphology 40:developed on top of a moving 274: 175: 161:, Andrew Goudie (Editor), 205: 204: 169:, Routledge, 2013 38:sedimentary basin 265: 226: 219: 212: 184: 177: 148: 142: 136: 135: 115: 26:thrust-sheet-top 273: 272: 268: 267: 266: 264: 263: 262: 258:Tectonics stubs 233: 232: 231: 230: 173: 152: 151: 143: 139: 117: 116: 112: 107: 94: 34:satellite basin 18:piggyback basin 12: 11: 5: 271: 269: 261: 260: 255: 250: 245: 235: 234: 229: 228: 221: 214: 206: 203: 202: 185: 171: 170: 156: 150: 149: 137: 126:(4): 475–478. 109: 108: 106: 103: 102: 101: 93: 90: 46:foreland basin 13: 10: 9: 6: 4: 3: 2: 270: 259: 256: 254: 251: 249: 248:Sedimentology 246: 244: 241: 240: 238: 227: 222: 220: 215: 213: 208: 207: 201: 199: 195: 192:article is a 191: 186: 183: 179: 174: 168: 164: 160: 157: 154: 153: 147: 141: 138: 133: 129: 125: 121: 114: 111: 104: 99: 98:Molasse basin 96: 95: 91: 89: 87: 83: 79: 75: 71: 66: 64: 60: 55: 51: 47: 44:as part of a 43: 39: 36:) is a minor 35: 31: 27: 23: 19: 198:expanding it 187: 172: 158: 140: 123: 119: 113: 86:Eastern Alps 80:in northern 72:in northern 67: 59:hanging wall 42:thrust sheet 33: 29: 25: 21: 17: 15: 237:Categories 167:041527298X 105:References 78:Ebro basin 22:piggy-back 253:Tectonics 190:tectonics 54:anticline 92:See also 70:Po basin 50:footwall 30:detached 120:Geology 63:orogeny 243:Basins 165:  20:(also 188:This 82:Spain 74:Italy 32:, or 194:stub 163:ISBN 128:doi 239:: 124:12 122:. 28:, 24:, 16:A 225:e 218:t 211:v 200:. 134:. 130::

Index

sedimentary basin
thrust sheet
foreland basin
footwall
anticline
hanging wall
orogeny
Po basin
Italy
Ebro basin
Spain
Eastern Alps
Molasse basin
doi
10.1130/0091-7613(1984)12<475:sbfacp>2.0.co;2

ISBN
041527298X
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tectonics
stub
expanding it
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e
Categories
Basins
Sedimentology
Tectonics
Tectonics stubs

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