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  2. Terrane - Wikipedia

    en.wikipedia.org/wiki/Terrane

    A tectonostratigraphic terrane is a fault-bounded package of rocks of at least regional extent characterized by a geologic history that differs from that of neighboring terranes. The essential characteristic of these terranes is that the present spatial relations are incompatible with the inferred geologic histories.

  3. Geology of Arkansas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Arkansas

    Oil exploration began in earnest in 1916 with an unsuccessful well east of El Dorado, in Union County (which at the time was known as Urbana County). A week after Samuel S. Hunter found modest amounts of oil in the Hunter No. 1 well near Stephens, Arkansas, the Constantin Oil and Refining Company found large amounts of oil and natural gas. Soon ...

  4. List of the Paleozoic life of Arkansas - Wikipedia

    en.wikipedia.org/wiki/List_of_the_Paleozoic_life...

    This list of the Paleozoic life of Arkansas contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of ...

  5. Paleontology in Arkansas - Wikipedia

    en.wikipedia.org/wiki/Paleontology_in_Arkansas

    Paleontology in Arkansas refers to paleontological research occurring within or conducted by people from the U.S. state of Arkansas. The fossil record of Arkansas spans from the Ordovician to the Eocene. [1] Nearly all of the state's fossils have come from ancient invertebrate life. [1] During the early Paleozoic, much

  6. Category:Terranes - Wikipedia

    en.wikipedia.org/wiki/Category:Terranes

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  7. Geology of North America - Wikipedia

    en.wikipedia.org/wiki/Geology_of_North_America

    Other Mesozoic terranes that accreted onto the continent include the Klamath Mountains, the Sierra Nevada, and the Guerrero super-terrane of western Mexico. [42] 80 to 90 million years ago the subducting Farallon plate split and formed the Kula Plate to the North. [32] Many of the major batholiths date from the late Cretaceous. [42]

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  9. Geology of the United States - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_United_States

    Today most Mesozoic and Cenozoic sedimentary rock layers that lie beneath much of the coastal plain and fringing continental shelf remain nearly horizontal or tilt gently toward the sea. [20] During the Cenozoic, the geology of the different regions diverged. The Appalachians started to uplift, while the Ouachita and Ozarks did not.