FACTOID # 19: Cheap sloppy joes: Looking for reduced-price lunches for schoolchildren? Head for Oklahoma!
 
 Home   Encyclopedia   Statistics   States A-Z   Flags   Maps   FAQ   About 
   
 
WHAT'S NEW
RELATED ARTICLES
People who viewed "Ophiolite" also viewed:
 

SEARCH ALL

FACTS & STATISTICS    Advanced view

Search encyclopedia, statistics and forums:

 

 

(* = Graphable)

 

 


Encyclopedia > Ophiolite

Ophiolites are sections of oceanic lithosphere that have been uplifted or emplaced to be exposed within continental crustal rocks. Examples include the Troodos Ophiolite in Cyprus, the Oman Ophiolite in the UAE, and Lizard Point in Cornwall, UK.


The stratigraphic sequence observed in ophiolites corresponds to the lithosphere-forming processes at mid-oceanic ridges:

SEDIMENTS: Muds (black shale) and cherts deposited since the crust formed.
EXTRUSIVE SEQUENCE: Basaltic pillow lavas show magma/seawater contact.
SHEETED DIKES: Vertical, parallel dikes which fed the pillow lavas above.
HIGH LEVEL INTRUSIVES: Gabbros, indicative of fractionated magma chamber.
CUMULATE SEQUENCE: Dunite-rich layers of unfractionated magma.
MANTLE SEQUENCE: Harzburgite/lherzolite-rich mantle rock.

The circulation of hydrothermal fluid through young oceanic crust causes alteration of the minerals observed: chlorite and serpentine, for example, in the sheeted dikes. Often, ore bodies such as iron-rich sulfide deposits are found above highly altered epidosites (epidote-quartz rocks) that are evidence of (the now relict) black smokers that continue to operate within the seafloor spreading centers of ocean ridges today.


Thus there is reason to believe that ophiolites are indeed oceanic mantle and crust; however, certain problems arise when looking closer... Compositional differences regarding silica content for example place ophiolite basalts in the domain of subduction zones (~55% silica) (whereas mid-ocean ridge basalts typically have a value ~50%). The crystallization order of feldspar and pyroxene in the gabbros is unexpectedly reversed, and ophiolites also appear to have a multi-phase magmatic complexity on par with subduction zones.


  Results from FactBites:
 
Ophiolites (421 words)
Ophiolites are pieces of oceanic plate that have been thrusted (obducted) onto the edge of continental plates.
Ophiolites are an assemblage of mafic and ultramafic lavas and hypabyssal rocks found in association with sedimentary rocks like greywackes and cherts.
Ophiolites are characterized by a classic sequence of rocks.
  More results at FactBites »

 
 

COMMENTARY     


Share your thoughts, questions and commentary here
Your name
Your comments

Want to know more?
Search encyclopedia, statistics and forums:

 


Press Releases |  Feeds | Contact
The Wikipedia article included on this page is licensed under the GFDL.
Images may be subject to relevant owners' copyright.
All other elements are (c) copyright NationMaster.com 2003-5. All Rights Reserved.
Usage implies agreement with terms, 1022, m