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  2. Terrane - Wikipedia

    en.wikipedia.org/wiki/Terrane

    In geology, a terrane (/ t ə ˈ r eɪ n, ˈ t ɛr eɪ n /; [1] [2] in full, a tectonostratigraphic terrane) is a crust fragment formed on a tectonic plate (or broken off from it) and accreted or "sutured" to crust lying on another plate. The crustal block or fragment preserves its distinctive geologic history, which is different from the ...

  3. Franciscan Complex - Wikipedia

    en.wikipedia.org/wiki/Franciscan_Complex

    Diagram (modified from Fig 3.11 in Irwin, 1990) showing the depositional setting of the Franciscan Assemblage and the contemporaneous Great Valley Sequence,. [ 5 ] The Franciscan Complex is an assemblage of metamorphosed and deformed rocks, associated with east-dipping subduction zone at the western coast of North America. [ 6 ]

  4. Metamorphic zone - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_zone

    When mapping the metamorphic grade of a terrane, a geologist has to take the lithology of the rock in account. Lithologies are mainly dependent on the protolith, the original rock before metamorphism. The main lithologies are ultramafic, mafic, felsic (or quartzo-feldspathic), pelitic and calcareous. In all of these (and other) lithologies ...

  5. Glossary of geology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_geology

    This glossary of geology is a list of definitions of terms and concepts relevant to geology, its sub-disciplines, and related fields. For other terms related to the Earth sciences , see Glossary of geography terms (disambiguation) .

  6. Wopmay orogen - Wikipedia

    en.wikipedia.org/wiki/Wopmay_orogen

    Geological map of north-western Canada. Wopmay orogen marked with D. The Wopmay orogen is a Paleoproterozoic orogenic belt in northern Canada which formed during the collision between the Hottah terrane (north of the Hottah Lake), a continental magmatic arc, and the Archean Slave Craton at about 1.88 Ga (billion years).

  7. Orogeny - Wikipedia

    en.wikipedia.org/wiki/Orogeny

    Orogeny (/ ɒ ˈ r ɒ dʒ ə n i /) is a mountain-building process that takes place at a convergent plate margin when plate motion compresses the margin. An orogenic belt or orogen develops as the compressed plate crumples and is uplifted to form one or more mountain ranges.

  8. Wrangellia terrane - Wikipedia

    en.wikipedia.org/wiki/Wrangellia_Terrane

    The term Wrangellia is confusingly applied to all of: The Wrangell(ia) Terrane alone; A composite terrane (CT) consisting of the Wrangell Terrane, Peninsular Terrane, and other rock units that were not originally part of the North American craton; A composite terrane which also includes the Alexander Terrane.

  9. Category:Terranes - Wikipedia

    en.wikipedia.org/wiki/Category:Terranes

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