Conventional accompaniments include rice, sliced tomatoes, onions, chopped fried plantains or fries and a glass or two called ” Lulada ” created using lulo fresh fruit, water and sugar.

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These times approximately delimit the Los Altares Member to 8. brand New constraints in the optimum depositional many years are provided here see after by the youngest U-Pb populations in 2 of y our detrital zircon examples: 8. These age that is u-Pb are in keeping with past geochronological outcomes, and verify a belated Miocene age for the Gigante development.

To look for the provenance regarding the Miocene Los Angeles Victoria, Villavieja, and Gigante Formations, modal compositional analyses of petrographic slim parts had been done for 15 sandstone examples through the north Los Angeles Venta and southern Gigante sections associated with Neiva Basin.

Slim parts had been stained for potassium and calcium feldspars to help in grain recognition. Main classifications are placed in Supplemental dining dining Table 3 3. The counts had been collected into composite metrics of quartz, feldspar, and different fractions that are lithic plotting on standard ternary diagrams Dickinson et al.

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Enigmatic microcrystalline grains with iron oxide staining included some doubt in differentiating aspects of the lithic small fraction, especially in terms of chert versus microcrystalline volcanic or metamorphic fragments. We concentrate on Q-F-Lf quartz—feldspar— Folk [] lithic fragments and Qm-F-Lt monocrystalline quartz—feldspar—total lithic fragments ternary diagrams Fig.

Examples throughout all three formations display heterogeneous compositions relatively evenly distributed among quartz, feldspar, and lithic fractions Figs. Many examples are classified as lithic chatroulette codes arkose or feldspathic litharenite Fig. an exclusion is uppermost Gigante sample S15, which exhibits the biggest quartz small fraction at Total feldspar is reasonably consistent through the entire Honda Group Los Angeles Victoria and Villavieja Formations , apart from sample S5, that will be significantly richer in plagioclase and nonvolcanic lithic fragments compared to the remaining portion of the Honda Group.

This test, from instantly underneath the Cerbatana Conglomerate during the Los Angeles Victoria—Villavieja contact , may emphasize a provenance modification for this transient shift in depositional conditions in charge of gravel input. In top stratigraphic amounts, less mature samples from the Gigante Formation S11—S15 are apt to have a lot higher proportions of volcanic lithic fragments and feldspars than examples through the underlying Honda Group Figs. Detrital zircon U-Pb geochronological analyses had been performed on 11 sandstone examples through the Neiva Basin; 7 Los Angeles Venta and four Gigante samples were crushed and zircon grains separated utilizing standard techniques, including water, heavy fluid, and separation that is magnetic.

A random choice of — zircons in each sample had been calculated via laser ablation—inductively combined plasma—mass spectrometry LA-ICP-MS in the University of Arizona LaserChron Center, after standard analytical procedures Gehrels et al.

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