enow.com Web Search

Search results

  1. Results from the WOW.Com Content Network
  2. Andesite - Wikipedia

    en.wikipedia.org/wiki/Andesite

    QAPF diagram with basalt/andesite field highlighted in yellow. Andesite is distinguished from basalt by SiO 2 > 52%. Andesite is field O2 in the TAS classification.. Andesite is an aphanitic (fine-grained) to porphyritic (coarse-grained) igneous rock that is intermediate in its content of silica and low in alkali metals.

  3. Andesite line - Wikipedia

    en.wikipedia.org/wiki/Andesite_line

    The andesite line is the most significant regional geologic distinction in the Pacific Ocean basin. It separates the mafic basaltic volcanic rocks of the Central Pacific Basin from the partially submerged continental areas of more felsic andesitic volcanic rock on its margins.

  4. Basaltic andesite - Wikipedia

    en.wikipedia.org/wiki/Basaltic_andesite

    The Columbia River Basalt Group is composed of 80% basaltic andesites on the basis of silicon content. Thick sequences of basaltic andesites were erupted in a shallow-marine environment during the Paleoproterozoic as melts formed in the anomalous Kaapval craton lithosphere. [10] The Mars Global Surveyor has found evidence for basaltic andesite ...

  5. Parinacota (volcano) - Wikipedia

    en.wikipedia.org/wiki/Parinacota_(volcano)

    Andesites from the old cone are classified as hornblende and pyroxene andesites. [1] Minerals found within the rocks include amphibole, apatite, biotite, clinopyroxene, iron oxide and titanium oxide, feldspar, olivine, orthopyroxene, pyroxene, sanidine and zircon. Not all of these minerals are found in rocks from all stages of Parinacota. [25]

  6. Lau Basin - Wikipedia

    en.wikipedia.org/wiki/Lau_Basin

    Lau Basin volcanics are mainly andesites and dacites that were erupted 6.4 to 9.0 Ma. Most mafic rocks found are 55% SiO2 basaltic andesites . [ 2 ] The whole basin floor is mostly composed of MORB-like rocks, but the westmost 80~120 km of the basin floor contains a mixture of MORB, transitional and arc-like basalts.

  7. Bearwallow Mountain Andesite - Wikipedia

    en.wikipedia.org/wiki/Bearwallow_Mountain_Andesite

    The Bearwallow Mountain Andesite is composed of calc-alkaline volcanic rock ranging from basaltic andesite to dacite, but predominantly andesite.These form a group of low cones or shield volcanoes and range in age from 27 to 23 million years old.

  8. Coromandel Volcanic Zone - Wikipedia

    en.wikipedia.org/wiki/Coromandel_Volcanic_Zone

    The Coromandel Volcanic Zone is generally older than the currently still active Hauraki and Taupō Rifts.This has implications as the widening of the Hauraki Rift was most about 5.5 million years ago, so the Kiwitahi volcanics (called by some the Kiwitahi Volcanic Zone), [4]: 16 which occur west of the Coromandel Peninsula and the Hauraki Rift are probably best regarded as related to the ...

  9. Dacite - Wikipedia

    en.wikipedia.org/wiki/Dacite

    The word dacite comes from Dacia, a province of the Roman Empire which lay between the Danube River and Carpathian Mountains (now modern Romania and Moldova) where the rock was first described. [ 1 ] The term dacite was used for the first time in the scientific literature in the book Geologie Siebenbürgens ( The Geology of Transylvania ) by ...