two-sheeted - significado y definición. Qué es two-sheeted
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Qué (quién) es two-sheeted - definición

SERIES OF PARALLEL DYKES CHARACTERISTIC OF OCEANIC CRUST
Sheeted dike comples; Sheeted dike complex; Sheeted dyke complexes; Sheeted dike complexes; Sheeted dyke; Sheeted dike
  • Cartoon to explain how one-sided chilled margins develop in sheeted dyke complexes from repeated intrusion at one location - four stages of intrusion are shown, with 1 being the earliest
  • (Top) Creation of [[rift valley]] due to low spreading rate. (Middle and bottom) Creation of [[mid-ocean ridge]]s due to higher spreading rate.<nowiki/>

Sheeted dyke complex         
A sheeted dyke complex, or sheeted dike complex, is a series of sub-parallel intrusions of igneous rock, forming a layer within the oceanic crust. At mid-ocean ridges, dykes are formed when magma beneath areas of tectonic plate divergence travels through a fracture in the earlier formed oceanic crust, feeding the lavas above and cooling below the seafloor forming upright columns of igneous rock.
Jacob Two-Two         
  • The cover of the first book of the series.
CANADIAN CHILDREN'S BOOK TRILOGY BY MORDECAI RICHLER, 1975 TO 1995 (OR SERIES INCLUDING ONE AUTHORIZED PREQUEL)
Jacob Twotwo; Jacob Two Two; Jacob Two-Two (character); Jacob Two Two Meets the Hooded Fang (book); Jacob Two-Two Meets the Hooded Fang (book)
Jacob Two-Two is a series of children's books written by Canadian author Mordecai Richler: Jacob Two-Two Meets the Hooded Fang (1975), Jacob Two-Two and the Dinosaur (1987) and Jacob Two-Two's First Spy Case (1995) written by Mordecai Richler, and Jacob Two-Two on the High Seas (2009) written by Cary Fagan.
Two-Mix         
JAPANESE POP DUO
TWO-MIX; Two Mix; II MIX DELTA
Two-Mix (temporarily known as II MIX⊿DELTA) is a Japanese pop duo formed in 1995 by Minami Takayama (vocals and composer) and Shiina Nagano (synthesizer, composer and lyricist). Their style is fast electronic pop.

Wikipedia

Sheeted dyke complex

A sheeted dyke complex, or sheeted dike complex, is a series of sub-parallel intrusions of igneous rock, forming a layer within the oceanic crust. At mid-ocean ridges, dykes are formed when magma beneath areas of tectonic plate divergence travels through a fracture in the earlier formed oceanic crust, feeding the lavas above and cooling below the seafloor forming upright columns of igneous rock. Magma continues to cool, as the existing seafloor moves away from the area of divergence, and additional magma is intruded and cools. In some tectonic settings slices of the oceanic crust are obducted (emplaced) upon continental crust, forming an ophiolite.