Possibility That Continental Lithosphere Is Involved in Subduction in Back-Arc Spreading

Shark, V. Ye.; Svalova, Valentina

doi:10.1080/00206819109465745

Cited by 4 publications

(3 citation statements)

References 9 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…adequate mechanical-mathematical model construction for the geological structures formation and evolution analysis is an important technique for the studies of velocity fields, stresses and temperatures in the sedimentary cover, crust and upper mantle at different tectonic conditions [8,9,[24][25][26][27][28][29][30]. It is possible to use two different approaches to mathematical modeling of geological structures and processes.…”

Section: Anmentioning

confidence: 99%

Geodynamics of Alpine Belt and Caribbean Region: Plate - Tectonics and Plume - Tectonics

Svalova

2022

J. Basic Appl. Sci.

View full text Add to dashboard Cite

The origin and evolution of geological structures reflect lithosphere-asthenosphere interaction in the process of lithospheric plate movement. Mantle diapirs contribute significantly to the sedimentary basins formation in Alpine belt and Caribbean region. Mantle diapirs are the result of density inversion in the asthenosphere–lithosphere system in the periods of tectonomagmatic activations. Increasing heat flow and mantle diapirs on the phone of convergence of Africa and Eurasia in Alpine belt and North and South Americas in Caribbean region produce intercontinental seas in the Cenozoic. The analytical solution of the problem give possibility to find the critical parameters connecting the mantle flow dynamics with surface relief evolution. In Alpine belt, the mantle diapirs form new basins at the final stage of Africa–Eurasia collision in the Cenozoic. In the Caribbean region, great mantle diapir separates the North and South Americas in the Mesozoic, and then the diapir is the source for different smaller diapirs during the convergence of these continents in the Cenozoic. The Gulf of Mexico and Pre-Caspian Depression are connected with mantle diapirs upwelling and have common geological-geophysical features as very rich oil-gas and salt bearing structures. Geodynamics of Alpine belt and the Caribbean region is determined by plume - tectonics on background of plate - tectonics in these regions.

show abstract

Section: Anmentioning

confidence: 99%

Geodynamics of Alpine Belt and Caribbean Region: Plate - Tectonics and Plume - Tectonics

Svalova

2022

J. Basic Appl. Sci.

View full text Add to dashboard Cite

show abstract

“…It is now known that this rectal gland Na + + K ++ + 2Cl − cotransporter is NKCC1, a product of the SLC12 gene family (SLC12A2; Hebert et al, 2004). The apical Cl − channel of the rectal gland displayed many of the electrical characteristics of the cystic fibrosus transmembrane conductance regulator (CFTR) when expressed in Xenopus oocytes by Mike Field's group (Sullivan et al, 1991) (not working at the MDIBL), and shark CFTR was cloned independently by two non-MDIBL groups (Grzelczak et al, 1990; Marshall et al, 1991). More recently, John Forrest's group at the MDIBL has cloned a K + channel from the rectal gland, which presumably mediates basolateral cycling of K + (Waldegger et al, 1999).…”

Section: The Shark Rectal Gland9mentioning

confidence: 99%

A brief history of fish osmoregulation: the central role of the Mt. Desert Island Biological Laboratory

Evans¹

2010

Front. Physio.

View full text Add to dashboard Cite

The Mt. Desert Island Biological Laboratory (MDIBL) has played a central role in the study of fish osmoregulation for the past 80 years. In particular, scientists at the MDIBL have made significant discoveries in the basic pattern of fish osmoregulation, the function of aglomerular kidneys and proximal tubular secretion, the roles of NaCl cotransporters in intestinal uptake and gill and rectal gland secretion, the role of the shark rectal gland in osmoregulation, the mechanisms of salt secretion by the teleost fish gill epithelium, and the evolution of the ionic uptake mechanisms in fish gills. This short review presents the history of these discoveries and their relationships to the study of epithelial transport in general.

show abstract

“…Accordingly, the continental material transported by the spreading plume head is expected to move in the same direction, where both material flows, migrating from the ocean and continental side consequently, will eventually collide. We consider the sequence of events on the basis of the mechanical-mathematical model for a multilayer viscous incompressible fluid, describing the dynamics of "granite" and "basalt" layers of the earth's crust, lithosphere, and asthenosphere (Sharkov, Svalova, 1991;2005). At the initial stages, when deflection of the layer boundaries from their original position is still insignificant, the base of the lithosphere always dives into the asthenosphere.…”

Section: Development Of Volcanic Arc -Backarc Systemsmentioning

confidence: 99%

Geological-Geomechanical Simulation of the Late Cenozoic Geodynamics in the Alpine-Mediterranean Mobile Belt

Шарков¹,

Svalova²

2011

New Frontiers in Tectonic Research - General Problems, Sedimentary Basins and Island Arcs

View full text Add to dashboard Cite

Possibility That Continental Lithosphere Is Involved in Subduction in Back-Arc Spreading

Cited by 4 publications

References 9 publications

Geodynamics of Alpine Belt and Caribbean Region: Plate - Tectonics and Plume - Tectonics

Geodynamics of Alpine Belt and Caribbean Region: Plate - Tectonics and Plume - Tectonics

A brief history of fish osmoregulation: the central role of the Mt. Desert Island Biological Laboratory

Geological-Geomechanical Simulation of the Late Cenozoic Geodynamics in the Alpine-Mediterranean Mobile Belt

Contact Info

Product

Resources

About