JIA Chengzao; ZHAO Wenzhi; WEI Guoqi; LIU Delai and ZHANG Junfeng
, 2003, 30(2): 282-0.
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Salt structures are widespread in North America, Africa, Europe, Southeast and Middle-east Asia, which are among the hottest topics of tectonic research and exploration for oil and gas during the annual meeting of AAPG in 2002. According to the latest researches, five stages have been found in the growth and development of salt structures, including early-stage diapir, local salt migration, coeval transformation of linear salt-walls, late-stage evolution of the mature diapirs and active diapiric episodes. During the evolution of the salt structures, eight types of structural styles can be recognized, such as salt walls, salt stock canopies and nappes, mini-basins, thrusts and strike-slip faults. With the applications of 3-D seismic and numerical modeling techniques, the growing stages and the tridimensional variation of salt structures should be able to be restored and recognized. Salt structures related with traps that are likely oil-bearing have been discovered recently in the Mexico Bay, Africa and Middle-east, which means that salt structures are closed are promising exploration areas of oil and gas, and they will play an important role in the growth of reserves.