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Wrinkle structures—a critical review

机译:皱纹结构-严格审查

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摘要

In this paper, a variety of so-called ‘wrinkle structures’ is reviewed in an attempt to help distinguish between crinkly decorations arising from physical processes that acted on siliciclastic bedding surfaces, and true microbially induced ‘wrinkle structures’. Two types of small-scale, microbially induced sedimentary structures are prominent due to their distinct geometry and mode of occurrence: (1) ‘elephant skin’ textures, characterized by reticulate patterns of sharp-crested ridges forming mm- to cm-scale polygons, occurring on argillite or argillaceous veneers above fine-grained sandstone and likely reflecting growth structures of microbial, mats (2) ‘Kinneyia’ structures, characterized by mm-scale flat-topped, winding ridges and intervening troughs and pits, sometimes resembling small-scale interference ripples. ‘Kinneyia’ structures usually occur on upper surfaces of siltstone/sandstone beds, themselves frequently event deposits, and are thought to have formed beneath microbial mats. Additionally, more linear variations of mat growth structures, partly resembling small-scale ‘α-petees’ may be developed. Finally, some wrinkly structures resulting from tractional mat deformation or mat slumping are occasionally preserved. These may appear as arcuate belts of non-penetrative, small-scale folds or as wrinkled bulges on otherwise flat surfaces.‘Wrinkle structures’ as indicators for the former presence of mats gain in importance if other mat-related structures are additionally observed in the same clastic succession, e.g. ‘sand chips’ (sandy intraclasts) or spindle-shaped or sinuously curved to circular sand cracks, frequently combined in networks. Furthermore, appropriate lithologies and facies are required. For instance, if compared with the distribution of modern cohesive microbial mats, laminated siltstone/argillite with intercalated siltstone/sandstone beds representing event deposits in tidal flat successions would be compatible with microbial mat development. Within a variety of physically induced small-scale wrinkly structures, miniature load structures may, above all, be misinterpreted as microbially induced ‘wrinkle structures’, due to their similar size and appearance, and their comparatively frequent occurrence.
机译:在本文中,对各种所谓的“皱纹结构”进行了综述,以试图区分由作用于硅质碎屑表面上的物理过程产生的皱纹装饰与真正的微生物诱导的“皱纹结构”。由于其独特的几何形状和发生方式,两种类型的由微生物引起的小规模沉积结构是突出的:(1)“象皮”纹理,其特征在于形成毫米至厘米级多边形的网状尖顶脊,发生在细粒砂岩上方的泥质微晶石或泥质胶合板上,可能反映了微生物,垫层的生长结构(2)“ Kinneyia”结构,其特征是毫米级的平顶,蜿蜒的山脊以及居间的谷和坑,有时类似于小规模干扰纹波。 “ Kinneyia”结构通常出现在粉砂岩/砂岩床的上表面,它们本身经常发生沉积,并被认为是在微生物垫下形成的。此外,可能会发展出垫子生长结构的更多线性变化,部分类似于小规模的“α-小蜂”。最后,偶尔会保留一些由于牵引垫变形或垫坍塌而产生的皱纹结构。这些可能表现为非穿透性,小规模褶皱的弓形带或在其他平坦表面上出现的皱纹凸起。相同的碎屑演替,例如“沙屑”(沙质碎屑)或纺锤形或弯曲成圆形的沙裂,经常组合成网状。此外,需要适当的岩性和相。例如,如果与现代粘性微生物垫的分布相比,层状粉砂岩/泥质岩与插层的粉砂岩/砂岩床层代表潮滩演替中的事件沉积物,将与微生物垫的发展兼容。在各种物理上引起的小规模皱纹结构中,由于它们的大小和外观相似,并且发生频率相对较高,因此,最重要的是,微型负载结构可能被误解为微生物引起的“皱纹结构”。

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