Crossword Solver > found answer > THINSKIN

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CROSSWORD
ANSWER

thinskin

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The answer THINSKIN has 6 possible clue(s) in existing crosswords.

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

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Definitions of thinskin in various dictionaries:

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Possible Crossword Clues
Oversensitive nature
Exterior for easily offended types
Feature of the easily offended
What an easily offended person has
Touchy nature
Super-sensitive nature

Last Seen in these Crosswords & Puzzles
Aug 9 2018 Eugene Sheffer - King Feature Syndicate
Jun 19 2017 New York Times
Jun 24 2016 USA Today
Feb 24 2015 Newsday.com
Feb 14 2014 Wall Street Journal
Feb 7 2012 New York Times

Thinskin 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.*

Thinskin 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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