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Convergent active margins are the most common type of active margin. Transform active margins are more rare, and occur when an oceanic plate and a continental plate are moving parallel to each other in opposite directions. These transform margins are often characterized by many offshore faults, which causes high degree of relief offshore ...
Most of these conventions are supported by active groups of map makers, and have been created and improved through long and serious discussions. The main intentions are: to display efficiently selected data; to create screen, web, print, creation & share friendly maps; to create a wiki style free of nationalism issues.
The following 15 pages use this file: Central America Volcanic Arc; Continental arc; EarthScope; Earth materials; Geology; Geology of the Rocky Mountains
A continental arc is a type of volcanic arc occurring as an "arc-shape" topographic high region along a continental margin.The continental arc is formed at an active continental margin where two tectonic plates meet, and where one plate has continental crust and the other oceanic crust along the line of plate convergence, and a subduction zone develops.
Maps showing a small geographic area should also have an inset locator map, locating that small geographic area in the context of a larger area, such as a continent or island chain. For example, see this map. Avoid blank space in the image around its main content to give the illusion of a margin around the image.
Most of the eastern Indian Ocean and nearly all of the Pacific Ocean margin are examples of active margins. While a weld between oceanic and continental lithosphere is called a passive margin, it is not an inactive margin. Active subsidence, sedimentation, growth faulting, pore fluid formation and migration are all active processes on passive ...
Usage: These maps are used especially by Template:Location map which uses geolocalisations to add a location mark (like ) and/or a label onto the map in the browser. They are also used as background for locator maps to enlight the place and area of major subdivisions in a country, of a species range, etc.
Sequence stratigraphy along the NE-SW transect as shown by green dotted line in the map above, modified after Hu et al. 2016. Detrital zircon age patterns (NW-SE): a transect of paleo-syncollisonal basins (59-56 Ma) on the active Asian continental margin, the point of collision and the passive Indian continental margin is considered. [5]
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