Sr, Nd, and Pb isotopic evidence for the origin and evolution of the Cántaro-Colima volcanic chain, Western Mexican Volcanic Belt

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Departamento de Sistemas Energéticos, Centro de Investigación en Energía, Universidad Nacional Autónoma de México, Priv. Xochicalco s/no., Col. Centro, Apartado Postal 34, Temixco, Mor. 62580, Mexico ^{[1
]}

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J. Volcanol. Geotherm. Res. | 1600年 / 1-4卷 / 33-51期

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[1] Sr, Nd, and Pb isotopic evidence for the origin and evolution of the Cantaro-Colima volcanic chain, Western Mexican Volcanic Belt
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[2] Geochemical and Sr-Nd isotopic evidence for a rift-related origin of magmas in Tizayuca Volcanic Field, Central Mexican Volcanic Belt
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[6] The origin of intraplate magmatism in the western Trans-Mexican Volcanic Belt
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[J]. GEOSPHERE, 2014, 10 (02): : 340 - 373
[7] Sr, Nd, and Pb isotopic and trace element geochemical constraints for a veined-mantle source of magmas in the Michoacan-Guanajuato Volcanic Field, west-central Mexican Volcanic Belt
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[J]. GEOCHEMICAL JOURNAL, 2004, 38 (01) : 43 - 65
[8] KINEMATIC EVOLUTION OF THE CONTINENTAL ACTIVE TRIPLE JUNCTION OF THE WESTERN MEXICAN VOLCANIC BELT
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[J]. COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II, 1991, 312 (02): : 135 - 142
[9] Geochemical and isotopic (Sr, Nd and Pb) characteristics of volcanic rocks from southwestern Ethiopia
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[10] ISOTOPIC AND TRACE-ELEMENT CONSTRAINTS ON THE ORIGIN AND EVOLUTION OF ALKALINE AND CALC-ALKALINE MAGMAS IN THE NORTHWESTERN MEXICAN VOLCANIC BELT
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