Results 161 to 170 of about 3,144 (230)

Submarine Landslides Induce Massive Waves in Subsea Brine Pools. [PDF]

Sci Rep, 2019
Sawyer DE, Mason RA, Cook AE, Portnov A.
europepmc   +1 more source

The structure of the Hallstatt evaporite body (Northern Calcareous Alps, Austria): A compressive diapir superposed by strike-slip shear?

J Struct Geol, 2014
Schorn A, Neubauer F.
europepmc   +1 more source

Sulphide Re-Os geochronology links orogenesis, salt and Cu-Co ores in the Central African Copperbelt. [PDF]

Sci Rep, 2018
Saintilan NJ, Selby D, Creaser RA, Dewaele S.   +3 more
europepmc   +1 more source

Fossil and present-day hydrotermal fluids from North Tunisia: an example of a dynamic fluid evolution [PDF]

, 2009
Charef, A., Guedes, Alexandra, Noronha, Fernando, Sousa, M.   +3 more
core   +1 more source

Assessing groundwater denitrification spatially is the key to targeted agricultural nitrogen regulation. [PDF]

Sci Rep
Hansen B, Aamand J, Blicher-Mathiesen G, Christiansen AV, Claes N, Dalgaard T, Frederiksen RR, Jacobsen BH, Jakobsen R, Kallesøe A, Kim H, Koch J, Møller I, Madsen RB, Schaper S, Sandersen PBE, Voutchkova DD, Wiborg I.   +17 more
europepmc   +1 more source

Erosion and diapirism: a comparitive analysis of salt diapirism for different cases of erosion

Tectonophysics, 1993
Poliakov, A., van Balen, R.T., Podlachikov, Y., Daudre, B., Cloetingh, S.A.P.L., Talbot, C.   +5 more
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Passive versus active salt diapirism

AAPG Bulletin, 2021
Existing definitions for passive and active salt diapirism are somewhat overlapping and ambiguous. These terms are also equated to downbuilding and upbuilding, respectively, which are problematic concepts as originally conceived and even as subsequently modified.
Mark G. Rowan, Katherine A. Giles
openaire   +1 more source

Mechanics of active salt diapirism

Tectonophysics, 1993
Abstract An active diapir forcefully intrudes its overburden, driven by diapir pressure that overcomes the resistance of the overburden strength. Possible causes for the driving pressure are differential loading of the source layer and a density contrast with the overburden.
D.D. Schultz-Ela, M.P.A. Jackson, B.C. Vendeville   +2 more
openaire   +1 more source

Megaflaps adjacent to salt diapirs

AAPG Bulletin, 2016
Megaflaps are steep stratal panels that extend far up the sides of diapirs or their equivalent welds. They have multiple-kilometer fold widths and structural relief and are thus distinct from smaller-scale composite halokinetic sequences. Maximum dips range from near-vertical to completely overturned.
Mark G. Rowan, Katherine A. Giles, Thomas E. Hearon IV, J. Carl Fiduk   +3 more
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Carbonate formation and alteration in the salt diapir caprock (Paskhand salt diapir, Southern Iran)

2023
The eastern Zagros Fold and Thrust Belt (ZFTB) in Iran includes a salt tectonic province with roughly 130 salt-gypsum diapirs emerging within the Neoproterozoic-Early Cambrian Hormuz Complex. The diapirs in the ZFTB differ in composition and in their distribution of exposed caprock mélanges (CRMs).
Sadegh Adineh, Prokop Zavada, Soraya Heuss-Aßbichler, Jiri Bruthans, Mathieu Daëron, Daniel A. Petrash   +5 more
openaire   +1 more source