22:
279:
226:
51:
263:
320:
211:
160:. That is, if a rock is sub-mature, then it has a much higher potential to generate further hydrocarbons than one that is overmature.
73:
199:
256:
354:
181:
van
Krevelen, D.W. (1950). "Graphical-statistical method for the study of structure and reaction processes of coal",
344:
313:
34:
349:
44:
38:
30:
249:
55:
339:
306:
169:
114:
87:
107:
290:
233:
95:
278:
333:
286:
103:
156:
The maturity of a source rock can also be used as an indicator of its hydrocarbon
130:
122:
118:
99:
232:
This article related to natural gas, petroleum or the petroleum industry is a
134:
225:
126:
15:
102:
generation. Maturity is established using a combination of
294:
237:
137:). Source rocks are therefore broadly categorised as
43:but its sources remain unclear because it lacks
314:
257:
8:
321:
307:
264:
250:
192:van Krevelen, D.W. and Schuyer, J. (1957)
200:The chemistry and technology of petroleum
153:(most hydrocarbons have been generated).
74:Learn how and when to remove this message
149:(extensive hydrocarbon generation) and
98:is a measure of its state in terms of
7:
275:
273:
222:
220:
212:Maturity (Maturation) Publications
145:(limited hydrocarbon generation),
14:
277:
224:
20:
121:), will alter under increasing
196:. Elsevier publishing company.
1:
141:(no hydrocarbon generation),
293:. You can help Knowledge by
236:. You can help Knowledge by
371:
272:
219:
29:This article includes a
58:more precise citations.
125:such that the organic
170:Van Krevelen diagram
115:total organic carbon
129:slowly mature into
355:Geochemistry stubs
31:list of references
345:Petroleum geology
302:
301:
245:
244:
88:petroleum geology
84:
83:
76:
362:
323:
316:
309:
281:
274:
266:
259:
252:
228:
221:
113:Rocks with high
79:
72:
68:
65:
59:
54:this article by
45:inline citations
24:
23:
16:
370:
369:
365:
364:
363:
361:
360:
359:
350:Petroleum stubs
330:
329:
328:
327:
271:
270:
217:
208:
178:
166:
108:basin modelling
80:
69:
63:
60:
49:
35:related reading
25:
21:
12:
11:
5:
368:
366:
358:
357:
352:
347:
342:
332:
331:
326:
325:
318:
311:
303:
300:
299:
282:
269:
268:
261:
254:
246:
243:
242:
229:
215:
214:
207:
206:External links
204:
203:
202:
197:
190:
177:
174:
173:
172:
165:
162:
82:
81:
39:external links
28:
26:
19:
13:
10:
9:
6:
4:
3:
2:
367:
356:
353:
351:
348:
346:
343:
341:
338:
337:
335:
324:
319:
317:
312:
310:
305:
304:
298:
296:
292:
289:article is a
288:
283:
280:
276:
267:
262:
260:
255:
253:
248:
247:
241:
239:
235:
230:
227:
223:
218:
213:
210:
209:
205:
201:
198:
195:
191:
188:
184:
180:
179:
175:
171:
168:
167:
163:
161:
159:
154:
152:
148:
144:
140:
136:
132:
128:
124:
120:
116:
111:
109:
105:
101:
97:
93:
89:
78:
75:
67:
57:
53:
47:
46:
40:
36:
32:
27:
18:
17:
340:Geochemistry
295:expanding it
287:geochemistry
284:
238:expanding it
231:
216:
194:Coal science
193:
186:
182:
157:
155:
150:
146:
142:
138:
131:hydrocarbons
119:source rocks
112:
110:techniques.
91:
85:
70:
61:
50:Please help
42:
123:temperature
104:geochemical
100:hydrocarbon
56:introducing
334:Categories
176:References
151:overmature
143:sub-mature
135:diagenesis
117:, (termed
189:, 269–84.
158:potential
127:molecules
64:June 2009
164:See also
139:immature
92:maturity
52:improve
147:mature
90:, the
285:This
133:(see
94:of a
37:, or
291:stub
234:stub
183:Fuel
106:and
96:rock
86:In
336::
187:29
185:,
41:,
33:,
322:e
315:t
308:v
297:.
265:e
258:t
251:v
240:.
77:)
71:(
66:)
62:(
48:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.