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Stratigraphy, sedimentology and structure of the Jurassic (Callovian to Lower Oxfordian) succession at Castle Hill, Scarborough, North Yorkshire, UK

机译:位于英国北约克郡斯卡伯勒城堡山的侏罗纪(Callovian到Lower Oxfordian)地层的地层学,沉积学和结构

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摘要

Site investigation borehole cores and temporary shaft exposures at the Toll House Pumping Station shaft site, Castle Hill, Scarborough, North Yorkshire, have revealed new data on the Callovian to Lower Oxfordian (Jurassic) succession. The condensed transgressive marine unit, the Lower Callovian Cornbrash Formation, rich in berthierine ooids and abundant shelly fossils, and the attenuated Cayton Clay Formation represent the Early Callovian marine transgression that flooded the low-gradient alluvial plain, which is represented by the underlying Scalby Formation. The Callovian Osgodby Formation (Red Cliff Rock and Langdale members) is an extensively bioturbated, silty sandstone with abundant berthierine–pyrite ooids in the lower part. It was deposited in lower- to upper-shoreface settings. Slow sedimentation rates, with long sediment residence time, resulted in a diverse ichnofauna and a high bioturbation index. Framboidal pyrite ooids in the lower Osgodby Formation sandstones are interpreted as being formed in anoxic lagoons in the nearshore zone; ooids were subsequently swept offshore during storm surge-ebb events. Cold water dinoflagellate cysts of Boreal affinity such as Gonyaulacysta dentata in the lower part of the Oxford Clay Formation indicate an Early Oxfordian age. This is confirmed by the presence of the zonal ammonite species Quenstedoceras mariae and is consistent with a relatively cold, but warming, palaeoclimate at this time. Shaft excavations revealed a new major fault, the Toll House Fault, which is interpreted to be a splay fault bifurcating off the main Castle Hill Fault. Together, the Toll House and Castle Hill faults form the western bounding faults of the Peak Trough, a graben-like structure that extends northwards, offshore.\ud\udSupplementary material: Supplementary data 1 (Macrofossil identifications from the Toll House shaft) and Supplementary data 2 (List of macropalaeontological specimens from the Toll House Boreholes) are available at https://dx.doi.org/10.6084/m9.figshare.c.3469968
机译:在北约克郡斯卡伯勒的卡斯尔希尔收费站抽水站竖井现场的现场调查井眼岩心和临时竖井暴露,揭示了从卡洛夫阶到下牛津阶(侏罗纪)的新数据。凝缩的海侵海单元,下卡洛夫康布拉什组,富含黄柏碱和丰富的贝壳化石,以及衰减的卡顿粘土组,代表了卡洛夫早期的海侵,淹没了低梯度冲积平原,这由下伏的斯卡比组所代表。 。卡洛夫的奥斯格比组(红崖岩和兰代尔成员)是一种生物扰动广泛的粉质砂岩,下部富含丰富的黄柏素-黄铁矿类化合物。它被沉积在下至上岸的环境中。沉积速度慢,沉积物停留时间长,导致鱼类鱼类种类繁多,生物扰动指数高。下奥斯格比地层砂岩中的片状黄铁矿卵石被解释为在近岸带的缺氧泻湖中形成。随后,在风暴潮-潮退事件中,阿片类物质被卷入海上。具有北方亲和力的冷水鞭毛藻囊,例如牛津黏土地层下部的齿齿扁豆(Gonyaulacysta dentata),表明牛津早期。这可以通过地带性铵石藻Quenstedoceras mariae的存在得到证实,这与此时相对寒冷但变暖的古气候相一致。竖井开挖揭示了一个新的主要断层,即收费站断层,这被解释为从主要城堡山断层分叉的八字形断层。收费站断层和城堡山断层共同构成了峰槽的西边界断层,这是一个向北延伸至近海的offshore形结构。数据2(收费站钻孔的宏观古生物学标本清单)可在https://dx.doi.org/10.6084/m9.figshare.c.3469968上获得。

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