Discussion and reply: Neogene volcanism at the front of the central Mexican Volcanic Belt: Basaltic andesites to dacites, with contemporaneous shoshonites and high-TiO2 lava - Discussion

Ignacio S. Torres-Alvarado; Surendra P. Verma

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Discussion and reply: Neogene volcanism at the front of the central Mexican Volcanic Belt: Basaltic andesites to dacites, with contemporaneous shoshonites and high-TiO2 lava - Discussion

机译：讨论和答复：墨西哥中部火山带前部的新近纪火山活动：玄武质安山岩至达西特岩质，同时有松山岩和高TiO2熔岩-讨论

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《GSA Bulletin》 |2003年第8期|1020-1021|共2页
作者
Ignacio S. Torres-Alvarado; Surendra P. Verma;
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Centro de Investigación en Energía, UNAM, Privada Xochicalco s, Centro, Temixco, 62580 Morelos, Mexico;

Centro de Investigación en Energía, UNAM, Privada Xochicalco s, Centro, Temixco, 62580 Morelos, Mexico;

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1. Discussion and reply: neogene volcanism at the front of the central mexican volcanic belt: basaltic andesites to dacites, with contemporaneous shoshonites and high-TiO_2 lava [J] . Ignacio S.Torres-Alvarado, Surendra P.Verma Geological Society of America Bulletin . 2003,第8期

机译：讨论和答复：墨西哥中部火山带前部的新近纪火山活动：玄武质安山岩至达菲斯岩，同时有松山岩和高TiO_2熔岩
2. Neogene volcanism at the front of the central Mexican volcanic belt: Basaltic andesites to dacites, with contemporaneous shoshonites and high-TiO2 lava [J] . Dawnika L. Blatter, Ian S.E. Carmichael, Alan L. Deino, GSA Bulletin . 2001,第10期

机译：墨西哥中部火山岩带前部的新近纪火山活动：玄武质安山岩至Dacites，同时有shoshonite和高TiO2熔岩
3. Neogene volcanism at the front of the central Mexican volcanic belt: Basaltic andesites to dacites, with cntemporaneous shoshonites and high-TiO_2 lava [J] . Dawnika L. Blatter, Ian S.E. Carmichael, Alan L. Deino, Geological Society of America Bulletin . 2001,第10期

机译：墨西哥中部火山岩带前部的新近纪火山作用：玄武质安山岩至Dacites，同时有长寿山岩和高TiO_2熔岩
4. Magmatic processes at the volcanic front of Central Mexican volcanic belt: Sierra de Chichinautzin volcanic field (Mexico) [O] . Velasco Tapia Fernando, Verma Surendra P. 2013

机译：中部墨西哥火山带的火山岩浆岩浆作用过程：墨西哥塞纳拉德奇亚努奇津火山场

Discussion and reply: Neogene volcanism at the front of the central Mexican Volcanic Belt: Basaltic andesites to dacites, with contemporaneous shoshonites and high-TiO2 lava - Discussion

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