Crossword Solver > found answer > THINSKINS

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ANSWER

thinskins

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The answer THINSKINS has 3 possible clue(s) in existing crosswords.

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The word THINSKINS is NOT valid in any word game. (Sorry, you cannot play THINSKINS in Scrabble, Words With Friends etc)

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Definitions of thinskins in various dictionaries:

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Possible Crossword Clues
Potato products that can't take criticism?
Outer onion features

Last Seen in these Crosswords & Puzzles
Aug 5 2014 Jonesin Crosswords
Jul 31 2014 Jonesin'
Jan 20 2013 Premier Sunday - King Feature Syndicate

Thinskins might refer to
Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks.The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc. This is particularly the case where a good basal decollement exists, usually in a weaker layer like a shale, evaporite, or a zone of high pore fluid pressure. This was first described in Rocky Mountains of the United States, as part of the Sevier Orogeny. * In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, you will see repeated sections of the same rock over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones.

Thinskins might refer to

Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks.The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc. This is particularly the case where a good basal decollement exists, usually in a weaker layer like a shale, evaporite, or a zone of high pore fluid pressure. This was first described in Rocky Mountains of the United States, as part of the Sevier Orogeny.
* In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, you will see repeated sections of the same rock over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones.

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