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Sedimentologic and diagenetic controls on pore-network characteristics of Oligocene-Miocene ramp carbonates (Majella Mountain, central Italy)

机译:渐新世-中新世斜坡碳酸盐岩孔隙网络特征的沉积学和成岩作用控制(意大利中部马杰拉山)

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This article addresses the controls exerted by sedimentologic and diagenetic factors on the preservation and modification of pore-network characteristics (porosity, pore types, sizes, shapes, and distribution) of carbonates belonging to the Bolognano Formation. This formation, exposed at the Majella Mountain, Italy, is composed of Oligocene-Miocene carbonates deposited in middle- to outer-ramp settings. The carbonates consist of (1) grainstones predominantly composed of either larger benthic foraminifera, especially Lepidocyclina, or bryozoans; (2) grainstones to packstones with abundant echinoid plates and spines; and (3) marly wackestones to mudstones with planktonic foraminifera.
机译:本文探讨了沉积学和成岩作用因素对博洛尼亚诺组碳酸盐岩孔隙网络特征(孔隙度,孔隙类型,大小,形状和分布)的保存和改变所施加的控制作用。该地层暴露于意大利的马耶拉山,由中斜至外斜坡的渐新世-中新世碳酸盐组成。碳酸盐由(1)主要由较大的底栖有孔虫,尤其是Lepidocyclina或苔藓虫组成的花岗石组成; (2)粒状到块状,具有丰富的棘突板和棘突; (3)泥灰质泥岩变为具有浮游有孔虫的泥岩。

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