Volcanic arc

Results: 260



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1JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B2, 2108, doi:2002JB001925, 2003  Volcanic and tectonic deformation on Unimak Island in the Aleutian Arc, Alaska Do¨rte Mann1 and Jeffrey Freymueller Geophysical In

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B2, 2108, doi:2002JB001925, 2003 Volcanic and tectonic deformation on Unimak Island in the Aleutian Arc, Alaska Do¨rte Mann1 and Jeffrey Freymueller Geophysical In

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Source URL: earthsci.stanford.edu

- Date: 2015-10-13 18:31:34
    2GEOPHYSICAL RESEARCH LETTERS, VOL. 29, NO. 16, 2001GL014088, 2002  Seismological evidence for a sub-volcanic arc mantle wedge beneath the Denali volcanic gap, Alaska Daniel E. McNamara USGS, Golden, CO, USA

    GEOPHYSICAL RESEARCH LETTERS, VOL. 29, NO. 16, 2001GL014088, 2002 Seismological evidence for a sub-volcanic arc mantle wedge beneath the Denali volcanic gap, Alaska Daniel E. McNamara USGS, Golden, CO, USA

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    Source URL: profile.usgs.gov

    - Date: 2012-02-22 17:18:10
      3NORTHWEST GEOLOGICAL SOCIETY A regional association of professionals, students & others interested in geology Please browse www.nwgs.org for more about us October 2014 Newsletter Volume 28, Number 6

      NORTHWEST GEOLOGICAL SOCIETY A regional association of professionals, students & others interested in geology Please browse www.nwgs.org for more about us October 2014 Newsletter Volume 28, Number 6

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      Source URL: www.nwgs.org

      Language: English - Date: 2016-05-16 00:57:46
      4The ophiolite problem: A perspective from drilling in the Western Pacific Sherman H. Bloomer, Department of Geosciences, Oregon State University Ophiolites are fragments of volcanic and plutonic rocks that have been used

      The ophiolite problem: A perspective from drilling in the Western Pacific Sherman H. Bloomer, Department of Geosciences, Oregon State University Ophiolites are fragments of volcanic and plutonic rocks that have been used

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      Source URL: www.odplegacy.org

      Language: English - Date: 2014-09-04 08:44:57
      5Generation of talc in the mantle wedge and its role in subduction dynamics in central Mexico

      Generation of talc in the mantle wedge and its role in subduction dynamics in central Mexico

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      Source URL: web.gps.caltech.edu

      Language: English - Date: 2013-11-08 17:58:38
      6doi:j.epsl

      doi:j.epsl

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      Source URL: www-udc.ig.utexas.edu

      Language: English - Date: 2013-12-27 00:50:42
      7Volcano When Pliny the Elder made his fateful journey across the Bay of Naples to Stabiae for a close-up view of the eruption, he invited his nephew, Gaius Plinius Secundus, better known as Pliny the Younger to accompany

      Volcano When Pliny the Elder made his fateful journey across the Bay of Naples to Stabiae for a close-up view of the eruption, he invited his nephew, Gaius Plinius Secundus, better known as Pliny the Younger to accompany

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      Source URL: www.huddarch.org.uk

      Language: English - Date: 2015-11-20 09:24:27
      89th International Symposium on Experimental Algorithms  May, 2010 – Hotel Continental Terme, Ischia (Naples), Italy  HOTEL CONTINENTAL TERME

      9th International Symposium on Experimental Algorithms May, 2010 – Hotel Continental Terme, Ischia (Naples), Italy HOTEL CONTINENTAL TERME

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      Source URL: www.sea2010.unina.it

      Language: English - Date: 2010-03-06 10:43:06
      9NORTHERN CALIFORNIA GEOLOGICAL SOCIETY  MEETING ANNOUNCEMENT NCGS Newsletter Editor: Dan Day:

      NORTHERN CALIFORNIA GEOLOGICAL SOCIETY MEETING ANNOUNCEMENT NCGS Newsletter Editor: Dan Day:

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      Source URL: www.ncgeolsoc.org

      Language: English - Date: 2010-11-16 21:45:55
      10news & views GEODYNAMICS Double dip  The Indian Plate moved north unusually quickly during the late Cretaceous. Numerical simulations suggest that this

      news & views GEODYNAMICS Double dip The Indian Plate moved north unusually quickly during the late Cretaceous. Numerical simulations suggest that this

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      Source URL: earth.usc.edu

      Language: English - Date: 2016-05-01 16:36:24