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Sources of dissolved silica to the fjords of northern Patagonia (44-48°S) : the importance of volcanic ash soil distribution and weathering

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Keywords
andosols, volcanic glass, northern Chilean Patagonia, dissolved silica, aquatic productivity, SOUTHERN-ANDES, SURFACE SEDIMENTS, CHILEAN PATAGONIA, LAKE-SEDIMENTS, TRACE-ELEMENT, GEOCHEMISTRY, ZONE, TEPHROCHRONOLOGY, PETROGENESIS, DEGLACIATION

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Citation

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MLA
Vandekerkhove, Elke, et al. “Sources of Dissolved Silica to the Fjords of Northern Patagonia (44-48°S) : The Importance of Volcanic Ash Soil Distribution and Weathering.” EARTH SURFACE PROCESSES AND LANDFORMS, vol. 41, no. 4, 2016, pp. 499–512, doi:10.1002/esp.3840.
APA
Vandekerkhove, E., Bertrand, S., Reid, B., Bartels, A., & Charlier, B. (2016). Sources of dissolved silica to the fjords of northern Patagonia (44-48°S) : the importance of volcanic ash soil distribution and weathering. EARTH SURFACE PROCESSES AND LANDFORMS, 41(4), 499–512. https://doi.org/10.1002/esp.3840
Chicago author-date
Vandekerkhove, Elke, Sebastien Bertrand, Brian Reid, Astrid Bartels, and Bernard Charlier. 2016. “Sources of Dissolved Silica to the Fjords of Northern Patagonia (44-48°S) : The Importance of Volcanic Ash Soil Distribution and Weathering.” EARTH SURFACE PROCESSES AND LANDFORMS 41 (4): 499–512. https://doi.org/10.1002/esp.3840.
Chicago author-date (all authors)
Vandekerkhove, Elke, Sebastien Bertrand, Brian Reid, Astrid Bartels, and Bernard Charlier. 2016. “Sources of Dissolved Silica to the Fjords of Northern Patagonia (44-48°S) : The Importance of Volcanic Ash Soil Distribution and Weathering.” EARTH SURFACE PROCESSES AND LANDFORMS 41 (4): 499–512. doi:10.1002/esp.3840.
Vancouver
1.
Vandekerkhove E, Bertrand S, Reid B, Bartels A, Charlier B. Sources of dissolved silica to the fjords of northern Patagonia (44-48°S) : the importance of volcanic ash soil distribution and weathering. EARTH SURFACE PROCESSES AND LANDFORMS. 2016;41(4):499–512.
IEEE
[1]
E. Vandekerkhove, S. Bertrand, B. Reid, A. Bartels, and B. Charlier, “Sources of dissolved silica to the fjords of northern Patagonia (44-48°S) : the importance of volcanic ash soil distribution and weathering,” EARTH SURFACE PROCESSES AND LANDFORMS, vol. 41, no. 4, pp. 499–512, 2016.
@article{7146945,
  author       = {{Vandekerkhove, Elke and Bertrand, Sebastien and Reid, Brian and Bartels, Astrid and Charlier, Bernard}},
  issn         = {{0197-9337}},
  journal      = {{EARTH SURFACE PROCESSES AND LANDFORMS}},
  keywords     = {{andosols,volcanic glass,northern Chilean Patagonia,dissolved silica,aquatic productivity,SOUTHERN-ANDES,SURFACE SEDIMENTS,CHILEAN PATAGONIA,LAKE-SEDIMENTS,TRACE-ELEMENT,GEOCHEMISTRY,ZONE,TEPHROCHRONOLOGY,PETROGENESIS,DEGLACIATION}},
  language     = {{eng}},
  number       = {{4}},
  pages        = {{499--512}},
  title        = {{Sources of dissolved silica to the fjords of northern Patagonia (44-48°S) : the importance of volcanic ash soil distribution and weathering}},
  url          = {{http://dx.doi.org/10.1002/esp.3840}},
  volume       = {{41}},
  year         = {{2016}},
}

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