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Evaluation of recent tectonomagmatic discrimination diagrams and their application to the origin of basic magmas in southern mexico and central america

机译:墨西哥南部和中美洲近期构造特征歧视图的评估及其在基本岩浆起源中的应用

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Discrimination diagrams to decipher tectonic settings have been in use for nearly 40 years. Although old diagrams have been extensively used, the recent ones based on discriminant functions of ratio variables, with or without log-transformation, proposed during 2004-2010 for the discrimination of four tectonic settings of island arc, continental rift, ocean-island and mid-ocean ridge, were newly evaluated to show their high success rates of 57.3-100% and 58.5-100% for major-element and immobile-element based diagrams, respectively. For the continental arc of the Andes evaluated for its similarity to island arc, these four sets of diagrams showed success rates of 62.1-83.8%. These four sets of five diagrams per set were therefore used to infer tectonic setting of the Mexican Volcanic Belt (MVB), Los Tuxtlas volcanic field (LTVF), and Central American Volcanic Arc (CAVA). Using this approach, the MVB, especially its western, central and eastern parts, and the LTVF of Southern Mexico show a dominantly continental rift setting and the CAVA shows an arc setting. The west-central part of the MVB is consistent with dual tectonics of arc and rift. These results confirm the application of an unusual mantle upwelling rift-model for the Mexican on-land volcanism, whereas the conventional plate tectonic subduction model seems to be applicable for the CAVA from Guatemala to north-western Costa Rica.
机译:用来区分构造环境的判别图已经使用了近40年。尽管已广泛使用旧图,但最近的图基于比例变量的判别函数(有或没有对数转换),于2004-2010年期间提出,用于区分岛弧,大陆裂谷,海洋岛和中部四个构造背景。最近对洋脊进行了评估,结果表明基于主要元素图和固定元素图的成功率分别为57.3-100%和58.5-100%。对于安第斯山脉的大陆弧与岛屿弧的相似性进行了评估,这四组图表显示成功率为62.1-83.8%。因此,这四套每套五张图被用来推断墨西哥火山带(MVB),洛斯图斯特拉斯火山场(LTVF)和中美洲火山弧(CAVA)的构造背景。使用这种方法,MVB(尤其是其西部,中部和东部)以及南墨西哥的LTVF表现出主要的大陆裂谷背景,而CAVA则显示了弧度背景。 MVB的中西部与弧和裂谷的双重构造一致。这些结果证实了不寻常的地幔上升裂谷模型在墨西哥陆上火山活动中的应用,而常规的板块构造俯冲模型似乎适用于从危地马拉到西北哥斯达黎加的CAVA。

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