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carbonates, evaporites and shales. Fold and thrusts have deformed all the Tajik
Depression rocks above the Jurassic salts. Tajikistan is highly seismically active, due to continued uplift, deformation and the underthrusting of the Eurasian continental crust 300 kilometers beneath the Pamir Mountains.
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are a high-altitude plateau region more than six kilometers above sea level, extending 400 kilometers by 225 kilometers. The Pamir
Mountains are tectonic belts, joined by suture features and trending from
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encompasses a nearly 90 percent mountainous landscape. The Tajik
Depression in the west is the only lowland in the entire country. The
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quartzose sediments and a two kilometer sequence of
Cretaceous to
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81:. Springer. p. 718.
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25:Trans-Altai Mountains
361:United Arab Emirates
388:limited recognition
29:Tien Shan Mountains
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485:Asia portal
386:States with
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246:South Korea
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18:geology of
366:Uzbekistan
341:Tajikistan
256:Kyrgyzstan
236:Kazakhstan
156:Bangladesh
146:Azerbaijan
64:References
53:Cretaceous
20:Tajikistan
452:Hong Kong
406:Palestine
331:Sri Lanka
326:Singapore
206:Indonesia
57:Oligocene
38:Paleozoic
500:Category
475:Category
396:Abkhazia
346:Thailand
301:Pakistan
281:Mongolia
276:Maldives
271:Malaysia
171:Cambodia
49:Jurassic
42:Cenozoic
371:Vietnam
286:Myanmar
266:Lebanon
196:Georgia
151:Bahrain
141:Armenia
416:Taiwan
351:Turkey
316:Russia
251:Kuwait
231:Jordan
221:Israel
181:Cyprus
166:Brunei
161:Bhutan
457:Macau
376:Yemen
336:Syria
311:Qatar
291:Nepal
226:Japan
201:India
191:Egypt
176:China
296:Oman
261:Laos
216:Iraq
211:Iran
16:The
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