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."
291:
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
146:
One source of different interpretations for a region stems from the fact that changes in different
47:
339:
88:
323:
227:
187:
61:
315:
292:
256:
195:
35:
119:
260:
168:
147:
333:
43:
278:
139:
131:
127:
123:
77:
319:
31:
17:
199:
210:
V.A. Obruchev (1948). "Osnovnye cherty kinetiki i plastiki neotektonik".
156:
135:
69:
247:
Pavlides, Spyros B. (1989). "Looking for a definition of neotectonics".
296:
152:
96:
81:
73:
39:
226:
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:βthe 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.β
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): 233β235.
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: 13β24
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:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.