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Neotectonics

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69:, 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 139:
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
73:. 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. 92:
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
89: 39:. The term may also refer to the motions/deformations in question themselves. Geologists refer to the corresponding time-frame as the 180: 84:"Neotectonics is the study of young tectonic events which have occurred or are still occurring in a given region after its 224: 220: 263: 100: 57:
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",
145: 124: 58: 141: 85: 70: 62: 28: 262: 175:"Encyclopedia of Coastal Science" (2005), Springer, 299:P. L. Hancock and G. D. Williams, "Neotectonics", 256: 23:, is the study of the motions and deformations of 107:β€œthe study of geologically recent motions of the 320: 96:Many researchers have accepted this approach. 183:, Chapter 1: "Tectonics and Neotectonics" 99:The Center for Neotectonic Studies at the 303:; March 1986; v. 143; no. 2; p. 325-326; 35:processes) that are current or recent in 235: 211: 209: 321: 115:, with the goals of understanding the 206: 131:hazard embodied in these processes.” 43:, and to the preceding time as the 13: 293: 250:10.1111/j.1365-3121.1989.tb00362.x 14: 340: 301:Journal of the Geological Society 111:, particularly those produced by 268:"Center for Neotectonic Studies" 274: 229: 193: 169: 88:or after its last significant 1: 163: 7: 201:Izv. Akad. Nauk, Ser. Geol. 151: 10: 345: 264:University of Nevada, Reno 123:recurrence, the growth of 101:University of Nevada, Reno 80:suggested the definition: 103:defines neotectonics as 309:10.1144/gsjgs.143.2.0323 133: 94: 189:10.1007/1-4020-3880-1 105: 82: 45:palaeotectonic period 19:, a subdiscipline of 225:Ch. 2: Neotectonics 286:10.1007/BF00563271 78:Spyros B. Pavlides 41:neotectonic period 181:978-1-4020-1903-6 51:Vladimir Obruchev 336: 313:article abstract 288: 278: 272: 271: 260: 254: 253: 233: 227: 213: 204: 197: 191: 173: 53:coined the term 33:geomorphological 344: 343: 339: 338: 337: 335: 334: 333: 319: 318: 296: 294:Further reading 291: 279: 275: 261: 257: 234: 230: 214: 207: 198: 194: 174: 170: 166: 154: 144:to the Miocene- 137:tectonic plates 90:tectonic set-up 12: 11: 5: 342: 332: 331: 317: 316: 295: 292: 290: 289: 273: 255: 244:(3): 233–235. 228: 205: 192: 167: 165: 162: 161: 160: 158:Seismic hazard 153: 150: 9: 6: 4: 3: 2: 341: 330: 327: 326: 324: 314: 310: 306: 302: 298: 297: 287: 283: 277: 269: 265: 259: 251: 247: 243: 239: 232: 226: 222: 221:0-19-927775-3 218: 212: 210: 202: 196: 190: 186: 182: 178: 172: 168: 159: 156: 155: 149: 147: 143: 138: 132: 130: 126: 122: 118: 114: 110: 109:Earth's crust 104: 102: 97: 93: 91: 87: 81: 79: 74: 72: 68: 65:) and in the 64: 60: 56: 52: 48: 46: 42: 38: 37:geologic time 34: 30: 26: 25:Earth's crust 22: 18: 300: 276: 258: 241: 237: 231: 200: 195: 171: 134: 106: 98: 95: 83: 75: 55:neotectonics 54: 49: 44: 40: 17:Neotectonics 16: 15: 113:earthquakes 238:Terra Nova 203:, 5: 13–24 164:References 148:boundary. 127:, and the 121:earthquake 67:Quaternary 29:geological 329:Tectonics 125:mountains 21:tectonics 323:Category 152:See also 146:Pliocene 76:In 1989 59:Tertiary 142:Miocene 129:seismic 117:physics 86:orogeny 71:Miocene 63:Neogene 219:  179:  217:ISBN 177:ISBN 31:and 305:doi 282:doi 246:doi 185:doi 119:of 47:. 325:: 266:. 240:. 223:, 208:^ 315:) 311:( 307:: 284:: 270:. 252:. 248:: 242:1 187:: 61:( 27:(

Index

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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