237:
211:
278:
190:"Long-term Creep of Rocks: Results with Large Specimens Obtained in about 20 Years and Those with Small Specimens in about 3 Years"
144:, is a geological material that behaves as a rheid over relatively short time-periods. As salt is buried by other types of
302:
271:
189:
133:
128:, it may be deduced that it is a solid and, therefore, behaving as a rheid when it undergoes said convection.
76:
under the given conditions. A material is a rheid by virtue of the time of observation. The term, coined by
264:
65:
297:
72:
during the time of observation is at least three orders of magnitude (1,000 ×) greater than the
25:
8:
161:
73:
244:
201:
149:
145:
117:
41:
141:
89:
77:
252:
248:
157:
101:
81:
291:
125:
69:
169:
105:
206:
121:
64:
is a substance whose temperature is below its melting point and whose
17:
165:
153:
136:
of about 4.5×10 Pa·s so it should be considered a rheid. Similarly
188:
Kumagai, Naoichi; Sadao
Sasajima; Hidebumi Ito (15 February 1978).
109:
85:
148:, it will often flow laterally towards regions of lower confining
124:
over long time-scales. As the mantle supports the propagation of
236:
187:
129:
32:
21:
137:
50:
113:
156:
and other structures may form. In some areas, such as the
53:
104:
can behave as a rheid under appropriate conditions of
56:
47:
194:
Journal of the
Society of Materials Science (Japan)
44:
24:. For places in Schleswig-Holstein in Germany, see
289:
272:
279:
265:
205:
290:
200:(293). Japan Energy Society: 157–161.
231:
13:
160:, these structures often serve as
95:
14:
314:
134:standard temperature and pressure
235:
40:
214:from the original on 2017-03-03
181:
1:
175:
251:. You can help Knowledge by
132:has a measured viscosity at
7:
152:. Through this mechanism,
10:
319:
230:
15:
303:Structural geology stubs
26:Rheide (disambiguation)
140:, the mineral form of
80:in 1953, has the same
16:For rhea-like birds (
112:. For example, the
92:and nonlinear flow.
243:This article about
207:10.2472/jsms.27.155
100:Almost any type of
74:elastic deformation
298:Structural geology
245:structural geology
260:
259:
88:, the science of
310:
281:
274:
267:
239:
232:
223:
222:
220:
219:
209:
185:
63:
62:
59:
58:
55:
52:
49:
46:
318:
317:
313:
312:
311:
309:
308:
307:
288:
287:
286:
285:
228:
226:
217:
215:
186:
182:
178:
98:
96:Types of rheids
90:viscoelasticity
78:S. Warren Carey
43:
39:
29:
12:
11:
5:
316:
306:
305:
300:
284:
283:
276:
269:
261:
258:
257:
240:
225:
224:
179:
177:
174:
158:Gulf of Mexico
97:
94:
9:
6:
4:
3:
2:
315:
304:
301:
299:
296:
295:
293:
282:
277:
275:
270:
268:
263:
262:
256:
254:
250:
246:
241:
238:
234:
233:
229:
213:
208:
203:
199:
195:
191:
184:
180:
173:
171:
167:
163:
159:
155:
151:
147:
143:
139:
135:
131:
127:
123:
119:
115:
111:
107:
103:
93:
91:
87:
83:
79:
75:
71:
67:
61:
38:
34:
27:
23:
19:
253:expanding it
242:
227:
216:. Retrieved
197:
193:
183:
99:
70:viscous flow
36:
30:
170:natural gas
126:shear waves
106:temperature
66:deformation
292:Categories
218:2008-06-16
176:References
154:salt domes
142:table salt
122:convection
120:undergoes
166:petroleum
146:sediments
212:Archived
110:pressure
86:rheology
84:root as
130:Granite
33:geology
22:Rheidae
20:), see
150:stress
138:halite
118:mantle
18:rheids
247:is a
162:traps
114:Earth
82:Greek
37:rheid
249:stub
168:and
164:for
108:and
102:rock
35:, a
202:doi
116:'s
68:by
31:In
294::
210:.
198:27
196:.
192:.
172:.
51:iː
280:e
273:t
266:v
255:.
221:.
204::
60:/
57:d
54:ɪ
48:r
45:ˈ
42:/
28:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.