Page 368 - Petroleum Geology
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            (1968)  studied  the  stratigraphy  around  the  salt  domes  and  found that in
            groups of salt domes that he called salt-stock .families, there was a sequential
            development from the “mother  salt stock” outwards in space and time (Fig.
            15-10), with progressively younger sedimentary rocks in the rim synclines. In
            this manner, he elucidated the development of the region (Fig. 15-11).
              In general, the development of  salt diapirs takes place during the accumu-
            lation and compaction of  the overlying sedimentary rocks, and so is contemp-
            oraneous with fluid expulsion from them.  The deformation of the sequence
            creates traps for any petroleum generated and expelled from the source rock;
            and ultimately such accumulations may be displaced to the flanks when pene-
            tration  of the overburden occurs. Because there is no known causal relation-
            ship between salt and petroleum, we  must regard these accumulations as co-
            incidental,  the  deformation  happening to take  place  while  petroleum was
            being generated. This is not necessarily true of mudstone diapirism.
              Mudstone diapirism has not received the same attention as salt diapirism,
            perhaps because it is not so distinctive; but it is probably more important in
            petroleum  geology  - particularly  the geology of  regressive sequences. This
            diapirism, from both  observational  and theoretical points of view, can begin
            soon after the more permeable, sandy, part of a regressive sequence begins to
            accumulate. Mud volcanism is mudstone diapirism at the surface, and incipient
            mudstone diapirism at depth is inferred for many parts of the world.
              The apparent rarity  of  penetrative mudstone diapirs at depth (but see Gil-
            reath,  1968; and  Bishop,  1978) and  their  common  occurrence  at  shallow
            depths is consistent with relative viscosity (and perhaps density) considerations
            because undercompaction is more pronounced at shallow depths. Mechanical
            instability in the sequence may remain  until the mudstone is buried under 4



            2 Generahon   1 Generation   2  Generation   3 Generatton   L Generation
                         (Master Salt Stock)


















            Fig.  15-10. Schematic diagram of development  of a salt-stock family. (After Sannemann,
            1968, p. 264, fig. 3.)
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