基于岩石学和岩石地球化学分析的河流沉积物对比研究方法建议:以lisama组新生代岩石(哥伦比亚中magdalena山谷)为例

J. Naranjo-Vesga, Pedro-David Gómez-Gutiérrez, Jaime-Ricardo Gélvez-Llanez, Noria-Elena Duque-Pardo, N. Moreno-Gómez
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引用次数: 2

摘要

对里萨马组河流沉积的岩石学和岩石地球化学分析表明,岩石的组成和化学变化可能与中马格达莱纳河谷盆地新生代地层单元的识别和对比有关。不同成分技术的综合应用使Lisama组被划分为三个岩相带。本文提出的分带与在同一地层剖面中定义的孢粉生物分带相匹配,显示了它们作为生物地层学补充对比工具的潜力。这种结合岩石学和岩石地球化学分析的方法可以用于中马格达莱纳盆地的后续研究,主要是在岩石形态恢复低或零的地理区域。本文将薄片分析、电感耦合等离子体光学发射光谱(ICP-OES)、电感耦合等离子体质谱(ICP-MS)和x射线衍射(XRD)技术集成到Nuevo Mundo向斜(NMS)东、西两翼两个相关的露头中。
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METHODOLOGY PROPOSAL FOR CORRELATION STUDIES OF FLUVIAL SEDIMENTS BASED ON PETROGRAPHIC AND LITHOGEOCHEMICAL ANALYSIS: EXAMPLE OF ITS APPLICATION ON CENOZOIC ROCK FROM THE LISAMA FORMATION (MIDDLE MAGDALENA VALLEY, COLOMBIA)
The petrographic and lithogeochemical analyses of fluvial sediments from the Lisama Formation suggest potential for the association of compositional and chemical changes of rocks with the identification and correlation of Cenozoic stratigraphic units in the Middle Magdalena valley basin. The integration of different compositional techniques enable the subdivision of the Lisama Formation into three petrographic zones. The zoning proposed herein match the palynological biozoning defined in the same stratigraphic sections, demonstrating their potential as a complementary correlation tool to biostratigraphy. This methodology of integrating petrographic and lithogeochemical analyses can be used in subsequent studies in the Middle Magdalena Basin, mainly in geographic areas where the palynomorph recovery is low or null. This work integrates Thin Section Analyses, Inductively Coupled Plasma Optical Emission Spectrometry (ICP-OES), Inductively Coupled Plasma Mass Spectrometry (ICP-MS) and X-Ray Diffraction (XRD) in two correlatable outcrops in the Western and Eastern flanks of the Nuevo Mundo Syncline (NMS).
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