Age and geochemistry of igneous rocks in the Guatemalan forearc: Implications for the early history of the Caribbean Large Igneous Province

危地马拉弧前火成岩的年龄和地球化学：对加勒比大型火成岩省早期历史的影响

• 批准号: 5434607
• 负责人: Professor Dr. Kaj Hoernle
• 金额: --
• 依托单位: Forschungseinheit Magmatische und Hydrothermale Systeme
• 依托单位国家: 德国
• 项目类别: Infrastructure Priority Programmes
• 财政年份: 2004
• 资助国家: 德国
• 起止时间: 2003-12-31 至 2007-12-31
• 项目状态: 已结题
• 来源: https://gepris.dfg.de/gepris/projekt/5434607?language=en
• 关键词: Age; geochemistry; igneous; rocks; Guatemalan

It is widely accepted that Large Igneous Provinces are formed through catastrophic magmatic events producing widespread volcanic plateaus within a relatively short period of time. One of the best-known examples is the Caribbean Large Igneous Province (CLIP). Recent geochronological and geochemical studies, however suggest that the CLIP represents an amalgamation of several smaller oceanic plateaus formed over long periods of time by multiple pulses of the Galápagos plume head. The vast ophiolitic basement beneath the Guatemalan forearc discovered and sampled during DSDP legs 67 and 84 could possibly represent an earlier part of such an oceanic plateau. We propose detailed geochronological, petrologic and geochemical investigations of samples from the drilling to confirm the possible affiliation of the 1000 km long forearc basement with the CLIP. The proposed study will not only expand our understanding of the temporal and geotectonic history of Central America, but also our knowledge of the age and composition of Large Igneous Provinces. A better understandig of how these provinces formed will allow us to better assess their impact on the past global enviroment and life on this planet.

人们普遍认为，大型火成岩省是通过在相对较短的时间内产生广泛的火山高原的灾难性岩浆事件而形成的，然而，最近的地质年代学和地球化学研究是最著名的例子之一。表明 CLIP 代表了几个较小的海洋高原的合并，这些高原是由加拉帕戈斯羽流头部的多次脉冲在长时间内形成的，下面是巨大的蛇绿岩基底。 DSDP 第 67 和 84 段期间发现并取样的危地马拉弧前可能代表了这样一个海洋高原的早期部分，我们建议对钻探样本进行详细的地质年代学、岩石学和地球化学研究，以确认 1000 公里长的弧前基底的可能归属。拟议的研究不仅将扩大我们对中美洲的时间和大地构造历史的了解，而且还将扩大我们对大型火成岩的年龄和成分的了解。更好地了解这些省份的形成方式将使我们能够更好地评估它们对过去的全球环境和地球上的生活的影响。