首页> 外文期刊>American Museum Novitates >The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)
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The Geology of Ukhaa Tolgod (Djadokhta Formation, Upper Cretaceous, Nemegt Basin, Mongolia)

机译:Ukhaa Tolgod的地质(蒙古内梅格特盆地上白垩统Djadokhta组)

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The lithostratigrahy and sedimentology of the fossiliferous Upper Cretaceous strata exposed in the Gobi Desert of Mongolia at Ukhaa Tolgod are described and mapped on aerial photos. Topographic features are also mapped by plane table and alidade.Five lithologic and sedimentologic facies are described: E-1, distinctly cross-stratified sandstone with fine structure, interpreted to represent eolian dune deposits; E-2, vaguely bedded sandstone with cross-stratified concretionary sheets, interpreted to represent eolian dune deposits modified by diagenetic formation of slope-parallel concretionary sheets of pedogenic calcite; S, structureless sandstone lacking concretions or cross-strata, interpreted to represent sandslide deposits generated by mass wasting along the lee slopes; C, conglomerate interpreted to represent basin-margin conglomerates washed into the dune field from adjacent topographic highs; and M, mudstone and siltstone interpreted to represent interdune deposition in ephemeral ponds and lakes. Facies E-2 and S have not been reported previously. Eleven stratigraphic sections at various localities within the Ukhaa Tolgod drainage basin are documented. The exposed composite section consists of about 75 m of pale orange sandstones, greenish-brown conglomerates, and brown siltstones that are products of an arid environment. Four schematic cross sections are documented to illustrate the lateral relationships among the five facies.
机译:描述并绘制了航拍照片,描绘了在乌卡阿托尔戈德蒙古戈壁沙漠暴露的化石上白垩纪地层的岩性和沉积学。地形特征还可以通过平面表和测井仪测绘。描述了五个岩性和沉积学相:E-1,明显为交叉分层的砂岩,具有精细的结构,被解释为代表风积沙丘沉积; E-2,层状含糊的交错层状含砂岩,解释为风成沙丘沉积物,由成岩方解石的斜坡平行含砾成岩作用成岩作用而形成。 S,无凝结物或交叉地层的无结构砂岩,被解释为代表由于沿下坡的质量浪费而产生的滑坡沉积物; C,砾岩解释为代表从邻近地形高处冲入沙丘场的盆地边缘砾岩; M,泥岩和粉砂岩被解释为代表临时池塘和湖泊中的砂岩沉积。先前尚未报道相E-2和S。记录了Ukhaa Tolgod流域内各个地方的11个地层剖面。裸露的复合部分包括约75 m的浅橙色砂岩,绿褐色的砾岩和棕色粉砂岩,它们是干旱环境的产物。记录了四个示意性横截面以说明五个相之间的横向关系。

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