17:
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level within the Zagros fold and thrust belt. The presence and thickness of the halites has had a major influence on the geometry of the thrust belt and such variations has been used to explain lateral changes in structural style along the belt.
164:
Smith A.G. (2012). "A review of the
Ediacaran to Early Cambrian ('Infra-Cambrian') evaporites and associated sediments of the Middle East". In Bhat G.M. (ed.).
110:. Two main depositional basins have been recognised, the North Gulf and South Gulf Basins, separated by the Qatar Arch. The basins were formed as a result of
91:
90:, the internal stratigraphy of the sequence is relatively poorly understood. They are the lateral equivalent of the evaporite-bearing Ara Group in the
228:"Effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: an analogue modelling approach"
195:
Talbot C.J.; Alvi M. (1996). "The past of a future syntaxis across the Zagros". In Alsop G.I.; Blundell D.J.; Davison I. (eds.).
134:
Most occurrences of the Hormuz
Formation are highly disturbed tectonically. However, a broad stratigraphy has been recognised.
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74:, a period previously referred to as the Infra-Cambrian. Most exposures of this sequence are in the form of emergent
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118:. The main structure formed during this period were NW-SE trending dextral (right lateral)
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Geology and
Hydrocarbon Potential of Neoproteozoic-Cambrian Basins in Asia
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Halite layers within the Hormuz sequence form the most important
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86:. As a result of their involvement in post-depositional
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The Hormuz
Formation is known from a wide area of the
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238:(5). London: Geological Society: 719–733.
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201:. Special Publications. Vol. 100.
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23:(dark grey areas) derived from Hormuz
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14:
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232:Journal of the Geological Society
226:Bahroudi, A.; Koyi H.A. (2003).
170:. Special Publications. London:
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62:that were deposited during the
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1:
150:
7:
287:Geologic formations of Iran
106:and around and beneath the
84:Zagros fold and thrust belt
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303:
138:Effect on Zagros structure
282:Geology of Saudi Arabia
244:10.1144/0016-764902-135
114:towards the end of the
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112:extensional tectonics
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174:. pp. 229–250.
205:. pp. 89–109.
122:and NE-SW trending
116:Pan-African Orogeny
203:Geological Society
172:Geological Society
124:extensional faults
120:strike-slip faults
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58:is a sequence of
52:Hormuz Evaporites
27:, extruding from
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256:
255:
223:
217:
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104:Zagros Mountains
92:South Oman Basin
44:Hormuz Formation
33:Zagros Mountains
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277:Geology of Iraq
272:Geology of Iran
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198:Salt Tectonics
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88:salt tectonics
72:Early Cambrian
68:Neoproterozoic
31:crests in the
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48:Hormuz Series
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21:Salt glaciers
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130:Stratigraphy
108:Persian Gulf
101:
98:Distribution
76:salt diapirs
56:Hormuz Group
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35:of southern
144:decollement
266:Categories
151:References
80:anticlines
60:evaporites
29:anticlinal
252:131504678
64:Ediacaran
82:of the
78:within
25:halites
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209:
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66:(Late
248:S2CID
70:) to
207:ISBN
176:ISBN
42:The
37:Iran
240:doi
236:160
54:or
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