Heldur Nestor, R. Einasto, V. Nestor, T. Märss, V. Viira
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引用次数: 12
摘要
描述了爱沙尼亚萨雷马岛西部Riksu钻井岩心的下Wenlock至中Ludlow段,包括Riksu组(Jaagarahu区域阶段,中Wenlock)的层型段。在类型剖面中重新定义了地层的下边界,并将其放置在Jaani地层的Paramaja段的顶部。建立了三个亚单元,即下、中、上日立层。描述了利苏组复杂的多期沉积旋回;中、次中、迷你和次迷你旋回暂时分别等于400、100、41和23 Ka milankovich旋回。Riksu组与爱沙尼亚的Jaagarahu、Muhu和Jamaja组以及哥特兰岛连续的Hogklint、Tofta (Kopparsvik)和Slite层大致相关。
DESCRIPTION OF THE TYPE SECTION, CYCLICITY, AND CORRELATION OF THE RIKSU FORMATION (WENLOCK, ESTONIA)
The lower Wenlock to middle Ludlow section of the Riksu drill core from western Saaremaa Island (Estonia), including the stratotype interval of the Riksu Formation (Jaagarahu Regional Stage, middle Wenlock) is described. The lower boundary of the formation is redefined in the type section and is placed on the top of the Paramaja Member of the Jaani Formation. Three subunits, the Lower, Middle, and Upper Riksu beds, are established. An intricate multistage sedimentary cyclicity of the Riksu Formation is described; the meso-, submeso-, mini-, and sub- minicycles are provisionally equated with 400, 100, 41, and 23 Ka Milankovitch cycles, respectively. The Riksu Formation is roughly correlated with its lateral equivalents - the Jaagarahu, Muhu, and Jamaja formations in Estonia, and with the successive upper Hogklint, Tofta (Kopparsvik), and Slite beds on Gotland.