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Neotectonics

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80:, which played an essential role in the origin of the contemporary topography". Since then geologists have disagreed as to how far back to date "geologically recent" time, with the common meaning being that neotectonics is the youngest, not yet finished stage in Earth tectonics. Some authors consider neotectonics to be basically synonymous with "active tectonics", while others date the start of the neotectonic period from the middle 150:
of the region may occur at different times, giving rise to the notion of the "transitional time", during which both palaeotectonic and neotectonic features coexist. For example, for central/northern Europe, the transitional period stretches from the middle early
84:. A general agreement has started to emerge that the actual time-frame may be individual for each geological environment and it must be set back in time sufficiently far to fully understand the current tectonic activity. 103:
The tectonic events are recent enough to permit a detailed analysis by differentiated and specific methods, while their results are directly compatible with seismological observations."
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A. Becker, " An attempt to define a "neotectonic period" for central and northern Europe", International Journal of Earth Sciences, Volume 82, Number 1, 1993
191: 50:. The term may also refer to the motions/deformations in question themselves. Geologists refer to the corresponding time-frame as the 231: 95:"Neotectonics is the study of young tectonic events which have occurred or are still occurring in a given region after its 235: 274: 111: 100: 68:
in his 1948 article, defining the field as "recent tectonic movements occurred in the upper part of
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One source of different interpretations for a region stems from the fact that changes in different
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V.A. Obruchev (1948). "Osnovnye cherty kinetiki i plastiki neotektonik".
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Pavlides, Spyros B. (1989). "Looking for a definition of neotectonics".
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Eduard A. Koster (2005) "The Physical Geography of Western Europe",
186:"Encyclopedia of Coastal Science" (2005), Springer, 310:P. L. Hancock and G. D. Williams, "Neotectonics", 34:, is the study of the motions and deformations of 118:β€œthe study of geologically recent motions of the 107:Many researchers have accepted this approach. 8: 194:, Chapter 1: "Tectonics and Neotectonics" 110:The Center for Neotectonic Studies at the 314:; March 1986; v. 143; no. 2; p. 325-326; 46:processes) that are current or recent in 222: 220: 179: 126:, with the goals of understanding the 7: 142:hazard embodied in these processes.” 54:, and to the preceding time as the 261:10.1111/j.1365-3121.1989.tb00362.x 25: 312:Journal of the Geological Society 122:, particularly those produced by 279:"Center for Neotectonic Studies" 99:or after its last significant 1: 212:Izv. Akad. Nauk, Ser. Geol. 356: 275:University of Nevada, Reno 134:recurrence, the growth of 112:University of Nevada, Reno 91:suggested the definition: 114:defines neotectonics as 320:10.1144/gsjgs.143.2.0323 144: 105: 200:10.1007/1-4020-3880-1 116: 93: 56:palaeotectonic period 30:, a subdiscipline of 236:Ch. 2: Neotectonics 297:10.1007/BF00563271 89:Spyros B. Pavlides 52:neotectonic period 192:978-1-4020-1903-6 62:Vladimir Obruchev 16:(Redirected from 347: 324:article abstract 299: 289: 283: 282: 271: 265: 264: 244: 238: 224: 215: 208: 202: 184: 64:coined the term 44:geomorphological 21: 355: 354: 350: 349: 348: 346: 345: 344: 330: 329: 307: 305:Further reading 302: 290: 286: 273: 272: 268: 246: 245: 241: 225: 218: 209: 205: 185: 181: 177: 165: 155:to the Miocene- 148:tectonic plates 101:tectonic set-up 23: 22: 15: 12: 11: 5: 353: 351: 343: 342: 332: 331: 328: 327: 306: 303: 301: 300: 284: 266: 255:(3): 233–235. 239: 216: 203: 178: 176: 173: 172: 171: 169:Seismic hazard 164: 161: 24: 14: 13: 10: 9: 6: 4: 3: 2: 352: 341: 338: 337: 335: 325: 321: 317: 313: 309: 308: 304: 298: 294: 288: 285: 280: 276: 270: 267: 262: 258: 254: 250: 243: 240: 237: 233: 232:0-19-927775-3 229: 223: 221: 217: 213: 207: 204: 201: 197: 193: 189: 183: 180: 174: 170: 167: 166: 162: 160: 158: 154: 149: 143: 141: 137: 133: 129: 125: 121: 120:Earth's crust 115: 113: 108: 104: 102: 98: 92: 90: 85: 83: 79: 76:) and in the 75: 71: 67: 63: 59: 57: 53: 49: 48:geologic time 45: 41: 37: 36:Earth's crust 33: 29: 19: 311: 287: 269: 252: 248: 242: 211: 206: 182: 145: 117: 109: 106: 94: 86: 66:neotectonics 65: 60: 55: 51: 28:Neotectonics 27: 26: 124:earthquakes 18:Neotectonic 249:Terra Nova 214:, 5: 13–24 175:References 159:boundary. 138:, and the 132:earthquake 78:Quaternary 40:geological 340:Tectonics 136:mountains 32:tectonics 334:Category 163:See also 157:Pliocene 87:In 1989 70:Tertiary 153:Miocene 140:seismic 128:physics 97:orogeny 82:Miocene 74:Neogene 230:  190:  228:ISBN 188:ISBN 42:and 316:doi 293:doi 257:doi 196:doi 130:of 58:. 336:: 277:. 251:. 234:, 219:^ 326:) 322:( 318:: 295:: 281:. 263:. 259:: 253:1 198:: 72:( 38:( 20:)

Index

Neotectonic
tectonics
Earth's crust
geological
geomorphological
geologic time
Vladimir Obruchev
Tertiary
Neogene
Quaternary
Miocene
Spyros B. Pavlides
orogeny
tectonic set-up
University of Nevada, Reno
Earth's crust
earthquakes
physics
earthquake
mountains
seismic
tectonic plates
Miocene
Pliocene
Seismic hazard
ISBN
978-1-4020-1903-6
doi
10.1007/1-4020-3880-1

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