Free thermohaline convection beneath allochthonous salt sheets: An agent for salt dissolution and fluid flow in Gulf Coast sediments

Publisher： John Wiley & Sons Inc

E-ISSN： 2156-2202|100|B9|18085-18092

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.100, Iss.B9, 1995-09, pp. : 18085-18092

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Abstract

Related content

Early Mesozoic rift stage half graben formation beneath the DeSoto Canyon salt basin, northeastern Gulf of Mexico

By  

Journal Of Geophysical Research, Vol. 100, Iss. B9, 1995-09 ,pp. : 17795-17812

John Wiley & Sons Inc

Access to resources Recommend Favorite

Quantification of thermal anomalies in sediments around salt structures

By Petersen K.   Lerche I.  

Geothermics, Vol. 24, Iss. 2, 1995-04 ,pp. : 253-268

Elsevier

Access to resources Recommend Favorite

Mercury volatilization from salt marsh sediments

By  

Journal Of Geophysical Research, Vol. 114, Iss. G2, 2009-06 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Salt dissolution and sinkhole formation along the Dead Sea shore

By  

Journal Of Geophysical Research, Vol. 111, Iss. B3, 2006-03 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Buoyancy‐driven propagation of isolated fluid‐filled fractures: Implications for fluid transport in Gulf of Mexico geopressured sediments

By  

Journal Of Geophysical Research, Vol. 101, Iss. B2, 1996-02 ,pp. : 2963-2970

John Wiley & Sons Inc

Access to resources Recommend Favorite