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Showing posts with label breccia. Show all posts
Showing posts with label breccia. Show all posts

Wednesday, October 4, 2017

Geologic Mélange: A Mixed Bag of Lithologies

      A geologic mélange consists of a jumble of large blocks of varied types of rocks.  A mélange is a large-scale breccia (rock consisting of angular fragments cemented together).  It is a mappable body of rock characterized by a lack of continuous bedding and the inclusion of fragments of rock of all different sizes, contained in a fine-grained deformed matrix.




       Large-scale mélanges formed in active continental margins generally consist of altered oceanic crustal material and blocks of continental slope sediments in a sheared mudstone matrix.






       The mixing mechanisms in such settings may include tectonic shearing forces, ductile flow of a water-charged or deformable matrix (such as serpentinite), 







and sedimentary action (such as slumping or gravity-flow). 






     Some larger blocks of rock may be as much as 1 kilometer (0.62 mi) across. Smaller-scale localized mélanges may also occur in shear or fault zones, where coherent rock has been disrupted and mixed by shearing forces.




      For my money, mélange is an beautiful-sounding word for a jumbled mess of lithologies. Sorting out environmental conditions in a mélange is a geological puzzle with well over 1,000 pieces.

Happy sorting and solving all those puzzle pieces!
Steph 

Deer and Dear Maizie---Fall in the Rockies: