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New Mexico Geological Society, 2023 Annual Spring Meeting, Proceedings Volume, Theme: "Geological responses to wildfires"最新文献

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The Uvas Basaltic Andesite: a Large-Volume Volcanic Field Erupted During the Initiation of the Southern Rio Grande Rift 乌瓦斯玄武岩安山岩:南里奥格兰德裂谷起始期爆发的大体积火山场
L. Hughes, Jeffery M. Amato
The Uvas Volcanic Field (UVF) is a large-volume dominantly mafic volcanic field representing the earliest (~27 Ma) significant mafic magmatism in the southern Rio Grande rift (RGR). It consists of lava flows, dikes, and domes with compositions ranging from basalt to trachyandesite. In this study, we will use 40 Ar/ 39 Ar dating, isotope (Nd and Pb) and whole-rock geochemistry, and geothermometry (olivine-liquid) to evaluate magma sources during the early stages of crustal extension in the southern RGR. We collected 32 samples over a broad area of the UVF, including the Sierra De Las Uvas Mtns, Goodsight Mtns., and Southern Caballo Mtns. Alteration is ubiquitous; to ensure accurate results, 10 of the least altered samples were subjected to ultrasonic leaching, crystal picking, and magnetic separation. Thin-sections from 16 samples show an assemblage mainly consisting of microlitic plagioclase, magnetite, and clinopyroxene, and medium-grained olivine and pyroxene phenocrysts. The samples show extensive alteration, with widespread secondary replacement of olivine and pyroxene, extensive clay development within plagioclase, and calcite-filled amygdules. Whole-rock geochemistry of 10 samples reveals a sub-alkaline character for the UVF with variations in SiO 2 (50–58 wt.%), Na 2 O (2.9–3.8 wt.%), and K 2 O (0.5–2.4 wt.%). Magma evolution was influenced by olivine and pyroxene fractionation, resulting in lower MgO, FeO, and CaO concentrations with increasing SiO 2 . Eight out of the ten samples generally show a depletion of high field-strength elements and an abundance of large-ion lithophile elements. The enrichment in mobile elements like Sr, Ba, and Pb, along with non-mobile elements such as Rb, despite being basaltic in composition, suggests significant crustal assimilation. Most UVF samples resemble basalts that come from modified sub-continental lithospheric mantle melting, similar to the Mogollon-Datil Volcanic field connected to the Cenozoic ignimbrite flare-up (~37–23 million years ago). Two samples from a location 30 km away (Southern Caballo Mtns.) from the main central domal uplift have an Ocean Island Basalt (OIB)-like composition, suggesting a different magma source. The origin of these samples, whether from a less-contaminated magma or a later pulse from a deeper source related to rapid extension in the Rio Grande rift beginning around 27 million years ago, remains uncertain. More radiogenic isotope analysis and precise dating will help clarify this. We will assess whether UVF's composition corresponds to the onset of rifting. By merging geochemical data with accurate 40 Ar/ 39 Ar dating, we aim to determine whether radiogenic isotope and geochemical signatures suggest a more primitive magma, as expected during widespread stretching in the eruptive period. Identifying a clear geochemical change from lithospheric mantle melting through conductive heating to asthenospheric melting through decompression melting would offer strong evidence f
乌瓦斯火山场(UVF)是南里约热内卢大裂谷(RGR)最早(~27 Ma)的显著基性岩浆活动,是一个以基性岩浆为主的大体积火山场。它由熔岩流、岩脉和圆顶组成,其成分从玄武岩到粗面山岩不等。本文将利用40 Ar/ 39 Ar定年、同位素(Nd和Pb)、全岩地球化学和地温(橄榄石-液体)等方法评价南缘RGR早期地壳伸展时期的岩浆来源。我们在广泛的UVF区域收集了32个样本,包括Sierra De Las Uvas Mtns, Goodsight Mtns。和南卡巴洛山脉。变化无处不在;为了确保准确的结果,10个变化最小的样品进行了超声波浸出,晶体采摘和磁选。16个样品的薄片显示其组合主要由微晶斜长石、磁铁矿和斜辉石以及中粒橄榄石和辉石斑晶组成。样品显示广泛的蚀变,广泛的橄榄石和辉石的二次替换,斜长石中广泛的粘土发育,以及方解石填充的杏仁体。10个样品的全岩地球化学特征表明,UVF呈亚碱性,sio2 (50 ~ 58 wt.%)、na2o (2.9 ~ 3.8 wt.%)和k2o (0.5 ~ 2.4 wt.%)含量变化。岩浆演化受橄榄石和辉石分馏作用影响,导致MgO、FeO和CaO浓度降低,sio2升高。10个样品中有8个普遍表现出高场强元素的耗竭和大离子亲石元素的丰富。富Sr、Ba、Pb等活动元素和Rb等非活动元素,尽管其成分为玄武岩,但表明明显的地壳同化作用。大多数UVF样品类似于来自改良的次大陆岩石圈地幔融化的玄武岩,类似于与新生代火成岩爆发(约3700万至2300万年前)有关的mogollong - datil火山场。两个样品来自30公里外(南卡巴洛Mtns)的主要中央穹隆隆起,具有类似海洋岛玄武岩(OIB)的成分,表明岩浆来源不同。这些样本的来源仍然不确定,究竟是来自污染较少的岩浆,还是来自与大约2700万年前开始的里约热内卢大裂谷快速伸展有关的更深层的岩浆脉冲。更多的放射性同位素分析和精确的年代测定将有助于澄清这一点。我们将评估UVF的组成是否与裂谷的开始相对应。通过将地球化学数据与精确的40 Ar/ 39 Ar测年相结合,我们的目标是确定放射性成因同位素和地球化学特征是否表明岩浆更原始,正如预期的那样在爆发期间广泛伸展。发现岩石圈地幔通过导电加热熔融到软流圈通过减压熔融熔融的明显地球化学变化,将为裂谷在~27 Ma左右开始提供有力的证据。我们的研究将有助于完善里约热内卢大裂谷早期岩浆生成的现有模型。
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of
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.
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引用次数: 0
期刊
New Mexico Geological Society, 2023 Annual Spring Meeting, Proceedings Volume, Theme: "Geological responses to wildfires"
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