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Salt dome

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to characterize subsurface geologic conditions and structures. Seismic reflection highlights the presence of a stark density contrast between the salt and surrounding sediment. Seismic techniques are particularly effective as salt domes are typically depressed blocks of crust bordered by parallel
310:, Texas. This led to the discovery of the first salt dome, revealed the importance of salt to the formation of hydrocarbon accumulations, and produced enough oil for petroleum to become an economically feasible fuel for the United States. Several countries use 230:. Some salt domes have salt sheets that extrude from the top of the dome; these are referred to as salt plugs. These plugs can coalesce to form salt canopies, which can then be remobilized by roof sedimentation, with the most prominent example in the northern 683:
Dronkert, H. & Remmelts, G. 1996. Influence of salt structures on reservoir rocks in Block L2, Dutch continental shelf. In: Rondeel, H.E., Batjes, D.A.J., Nieuwenhuijs, W.H. (eds): Geology of gas and oil under the Netherlands, Kluwer (Dordrecht):
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salt forms salt domes in the Essaouira Basin onshore and offshore Morocco. An equivalent salt sequence, the Argo Formation, is associated with salt dome formation on the conjugate
149:, it is recognized that a single evaporation event is rarely enough to produce the vast quantities of salt needed to form a layer thick enough for the formation of salt 282:
provinces. The rock salt of the salt dome is mostly impermeable, so, as it moves up towards the surface, it penetrates and bends existing rock along with it. As
555:(Lower Cretaceous) age salt was deposited within the area of thinned crust on both the Brazilian and conjugate Angola/Gabon margins forming many salt domes. 536: 618:
Schreiber, B.C. and Hsü, K.J. (1980) Evaporites. In Developments in Petroleum Geology, Vol. 2 (Ed. G.D. Hobson), pp. 87–138. Elsevier Science, Amsterdam.
172:, thereby creating a salt diapir. However, after the 1980s, the primary force that drives the flow of salt is considered to be differential loading. 198:, ductile thinning, or other forms of regional deformation. The vertical growth of salt formations creates pressure on the upward surface, causing 1002: 968: 782: 1332: 315: 435:
near Moab, Utah. A Paradox Formation salt body that has risen as a ridge through several hundred meters of overburden, predominantly
906: 905: 1284: 996: 868:. Encyclopedia of Earth, eds. A.Jorgensen and C.J.Cleveland, National Council for Science and the environment, Washington DC 397: 238:. These occur when the growth of a dome is prevented by an exhausted supply of salt, and the top and bottom contacts merge. 1008: 1363: 594: 91:. Salt domes can have unique surface and subsurface structures, and they can be discovered using techniques such as 1462: 840: 381:. The thicker salt is found in a series of basins: the Western Gulf, the Southern Gulf, and the Oman salt basins. 190:). The flow of the salt overcomes the strength of the overburden as well as boundary friction aided by overburden 1502: 961: 940: 798: 564: 210:
where the accumulation of sediments around the diapir contribute to its growth and eventually form into a dome.
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Salt domes occur in many parts of the world where there is a sufficiently thick layer of rock salt developed.
249:. The latter was developed based on techniques from the former and is more effective. Seismic refraction uses 1018: 464: 405: 389: 219: 179: 1358: 1279: 844: 183: 175: 882: 164:. Previously, researchers believed that the compaction of overlying sediment and subsequent decrease in 1307: 1246: 286:
of rock are penetrated, they are, generally, bent upwards where they meet the dome, forming pockets and
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Some salt domes can be seen from Earth's surface. They can also be located by finding unique
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dried out. Later deposition, once the sea refilled, triggered the formation of salt domes.
443:(arching upward along its center line) which fractured and eroded to expose the salt body. 1430: 1425: 1302: 1269: 1226: 1201: 1176: 991: 529: 307: 303: 255: 206:. Once the salt completely pierces the overburden, it can rise through a process known as 187: 31: 817: 654: 1420: 1337: 1259: 1181: 1121: 1066: 1061: 1013: 522: 517: 506: 499: 362: 330: 299: 235: 223: 120: 100: 80: 724: 393:
End-on view of emergent Onion Creek salt dome between remnants of displaced overburden
341:, and other substances, which can be used in products such as table salt and chemical 60: 1486: 1384: 1264: 1211: 1161: 740: 480: 460: 432: 413: 311: 142: 65: 864: 825: 662: 1410: 1231: 1186: 1126: 1111: 1046: 774: 589: 568: 370: 334: 267: 250: 195: 146: 133:. The formation of a salt dome begins with the deposition of salt in a restricted 904: 762: 1476: 1312: 1274: 1236: 1221: 1196: 1156: 1146: 1116: 1096: 1091: 1086: 1076: 532: 503: 452: 401:
Lateral view of emergent salt dome from ridge of remnant of displaced overburden
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and surrounding phenomena. For instance, salt domes can contain or be near
141:, resulting in the precipitation and deposition of salt. While the rate of 17: 1435: 1216: 1206: 1071: 421: 203: 165: 157: 924:
was created from a revision of this article dated 26 July 2019
765:, in Harff, Jan; Meschede, Martin; Petersen, Sven; Thiede, Jörn (eds.), 1254: 1131: 797:
Thomas R.; Ellison R.A.; Goodenough K.M.; Roberts N.; Allen P. (2015).
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Schultz-Ela, D.D; Jackson, M.P.A; Vendeville, B.C. (January 12, 1992).
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is associated with widespread salt dome formation in most parts of the
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of salt is significantly larger than the rate of sedimentation of
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led to salt rising and intruding into the overburden due to its
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efforts led to the discovery of numerous salt domes soon after
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Stratigraphically, salt basins developed periodically from the
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For the domed buildings sometimes used to store rock salt, see
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An example of an emergent salt dome is at Onion Creek, Utah /
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minerals) intrudes into overlying rocks in a process known as
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The Gulf Coast is home to over 500 salt domes formed from
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Group has formed salt domes over the central and southern
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caverns for holding large amounts of oil or gas reserves
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Over time, the layer of salt is covered with deposited
841:"Geosights: The Onion Creek salt diapir, Grand County" 763:"Salt Diapirism in the Oceans and Continental Margins" 234:. Another structure that can form from salt domes are 1460: 325:
above the salt domes can contain deposits of native
302:. In 1901, an exploratory oil well was drilled into 1403: 1377: 1346: 1293: 1245: 1037: 984: 883:Salt Dome Cutaway - Louisiana State Exhibit Museum 439:. As the salt body rose, the overburden formed an 769:, Dordrecht: Springer Netherlands, pp. 1–8, 637:Hudec, Michael R.; Jackson, Martin P. A. (2007). 278:Salt domes are the site of many of the world's 463:salt was deposited, forming salt domes in the 160:, becoming buried under an increasingly large 962: 639:"Terra infirma: Understanding salt tectonics" 451:Offshore northern Norway in the southwestern 333:). They can also contain deposits of metals, 8: 551:During the break-up of the south Atlantic, 182:), forced displacement of salt boundaries ( 969: 955: 947: 932:, and does not reflect subsequent edits. 915: 700:"What is a Salt Dome? How do they form?" 571:), thick salt layers were formed as the 241:Salt domes have also been located using 36: 27:Structural dome formed of salt or halite 1467: 1003:International Salt Co. v. United States 611: 178:can be caused by gravitational forces ( 115:Diagram showing formation of salt domes 521:Imaging of undersea salt domes in the 416:in the US, which extends from eastern 45:(the white area in the middle) in the 756: 754: 752: 750: 535:. This region is home to most of the 7: 1333:List of countries by salt production 725:"Mechanics of Active Salt Diapirism" 694: 692: 690: 632: 630: 628: 626: 624: 491:, extending eastwards into Germany. 767:Encyclopedia of Marine Geosciences 25: 1470: 1447: 1446: 914: 412:forms salt domes throughout the 1285:Salt and cardiovascular disease 826:10.1016/j.precamres.2014.10.011 663:10.1016/j.earscirev.2007.01.001 775:10.1007/978-94-007-6644-0_93-1 537:US Strategic Petroleum Reserve 361:In the Middle East, the upper 1: 741:10.1016/0040-1951(93)90345-k 595:Underground hydrogen storage 761:Drachev, Sergey S. (2014), 735:(3–4). Amsterdam: 275–312. 543:was formed by a salt dome. 373:and onshore in Iran, Iraq, 83:formed when salt (or other 1529: 547:South Atlantic salt basins 118: 29: 1444: 997:In the American Civil War 565:Messinian salinity crisis 186:), or thermal gradients ( 41:Astronaut photography of 1303:Salt Industry Commission 99:as they can function as 95:. They are important in 863:C.Michael Hogan. 2011. 420:, through southwestern 910: 890:Listen to this article 845:Utah Geological Survey 525: 402: 394: 116: 72: 57: 909: 643:Earth-Science Reviews 520: 400: 392: 264:petroleum exploration 180:gravitational loading 114: 63: 40: 1328:Open-pan salt making 1152:Monosodium glutamate 941:More spoken articles 806:Precambrian Research 585:Plasticity (physics) 479:In northwest Europe 375:United Arab Emirates 232:Gulf of Mexico basin 214:Discovery mechanisms 184:displacement loading 176:Differential loading 839:McCalla C. (2008). 818:2015PreR..256....1T 655:2007ESRv...82....1H 495:Morocco–Nova Scotia 457:Upper Carboniferous 1167:Potassium chloride 1019:In Chinese history 911: 600:Gorleben salt dome 526: 424:into northwestern 403: 395: 329:(recovered by the 247:seismic reflection 243:seismic refraction 220:surface structures 117: 93:seismic reflection 73: 58: 1458: 1457: 1395:Salting the earth 1390:Salt in the Bible 1364:San Francisco Bay 1172:Potassium nitrate 907: 784:978-94-007-6644-0 573:Mediterranean Sea 410:Paradox Formation 228:natural gas vents 208:passive diapirism 97:petroleum geology 16:(Redirected from 1520: 1503:Economic geology 1475: 1474: 1466: 1450: 1449: 1308:Evaporation pond 1082:Calcium chloride 971: 964: 957: 948: 931: 929: 918: 917: 908: 898: 896: 891: 870: 861: 855: 854: 852: 851: 843:. Survey Notes. 836: 830: 829: 803: 794: 788: 787: 758: 745: 744: 720: 714: 713: 711: 710: 696: 685: 681: 675: 674: 634: 619: 616: 408:age salt of the 367:Hormuz Formation 357:Hormuz Formation 300:petroleum traps) 51:Bushehr Province 47:Zagros Mountains 43:Jashak salt dome 21: 1528: 1527: 1523: 1522: 1521: 1519: 1518: 1517: 1498:Salt production 1483: 1482: 1481: 1469: 1461: 1459: 1454: 1440: 1431:Ximenes Redoubt 1426:Water softening 1399: 1373: 1342: 1295: 1289: 1270:Salt-cured meat 1241: 1227:Sodium chloride 1202:Salt substitute 1177:River reed salt 1033: 980: 975: 945: 944: 933: 927: 925: 922:This audio file 919: 912: 903: 900: 894: 893: 889: 879: 874: 873: 862: 858: 849: 847: 838: 837: 833: 801: 796: 795: 791: 785: 760: 759: 748: 722: 721: 717: 708: 706: 698: 697: 688: 682: 678: 636: 635: 622: 617: 613: 608: 581: 561: 549: 530:Middle Jurassic 515: 497: 477: 475:Zechstein basin 449: 387: 359: 351: 312:solution mining 304:Spindletop Hill 276: 274:Commercial uses 216: 188:thermal loading 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dome in 62: 56: 52: 48: 44: 39: 33: 19: 1411:Mineral lick 1296:and industry 1112:Fleur de sel 1001: 865: 859: 848:. 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Index

Salt diapir
Monolithic dome

Jashak salt dome
Zagros Mountains
Bushehr Province
Iran

Fars Province
Iran
structural dome
evaporite
diapirism
seismic reflection
petroleum geology
petroleum traps

Salt tectonics
Proterozoic
Neogene
basin
evaporation
sedimentation
clastics
diapirs
sediment
overburden
buoyancy
ductility
Differential loading

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