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Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas

(2006) CHEMICAL GEOLOGY. 233(3-4). p.346-357
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Chicago
KAMENETSKY, VS, Marlina Elburg, R ARCULUS, and R THOMAS. 2006. “Magmatic Origin of low-Ca Olivine in Subduction-related Magmas: Co-existence of Contrasting Magmas.” Chemical Geology 233 (3-4): 346–357.
APA
KAMENETSKY, V., Elburg, M., ARCULUS, R., & THOMAS, R. (2006). Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas. CHEMICAL GEOLOGY, 233(3-4), 346–357.
Vancouver
1.
KAMENETSKY V, Elburg M, ARCULUS R, THOMAS R. Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas. CHEMICAL GEOLOGY. Elsevier Science; 2006;233(3-4):346–57.
MLA
KAMENETSKY, VS, Marlina Elburg, R ARCULUS, et al. “Magmatic Origin of low-Ca Olivine in Subduction-related Magmas: Co-existence of Contrasting Magmas.” CHEMICAL GEOLOGY 233.3-4 (2006): 346–357. Print.
@article{351183,
  author       = {KAMENETSKY, VS and Elburg, Marlina and ARCULUS, R and THOMAS, R},
  issn         = {0009-2541},
  journal      = {CHEMICAL GEOLOGY},
  language     = {eng},
  number       = {3-4},
  pages        = {346--357},
  publisher    = {Elsevier Science},
  title        = {Magmatic origin of low-Ca olivine in subduction-related magmas: Co-existence of contrasting magmas},
  volume       = {233},
  year         = {2006},
}

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