首页> 外文期刊>Annals Of Geophysics >A rare Mid-Würmian lithoid tuff in the Agro Pontino graben (Southern Lazio, Italy) and its identification as an Albano 5-7 related distal tephra deposit (41-36 kaBP): characteristics, provenance and palaeogeographical implications
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A rare Mid-Würmian lithoid tuff in the Agro Pontino graben (Southern Lazio, Italy) and its identification as an Albano 5-7 related distal tephra deposit (41-36 kaBP): characteristics, provenance and palaeogeographical implications

机译:Agro Pontino en石(意大利南拉齐奥)中稀有的中乌尔姆阶类固醇凝灰岩,并被鉴定为与阿尔巴诺5-7相关的远缘特非拉沉积物(41-36 kaBP):特征,物源和古地理意义

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摘要

A lithoid tuff, found in 2011 (Ricci pit, Agro Pontino, Southern Lazio, Italy), was studied for its composition, origin and palaeogeographical implications. This tuff was the first occurrence of a Würmian-age tephra layer, encountered in the coastal basins of Southern Lazio. Based on its mineralogy and isotopic composition (Sr and Nd), it was identified as a distal tephra deposit from the Volcano Laziale, connected with the Albano 6-7 eruptive phase (‘Lapis Albanus’) and dating from 41-36 ka BP. The lithoid tuff consists of tephra that were slightly reworked and subsequently lithified, when this central part of the Agro Pontino graben still consisted of a non-dissected, level lagoonal plain. The study confirms the earlier established importance of this tephra layer as stratigraphic marker for Central Italy, and shows that its distribution is wider than earlier assumed, notably to the SE of the Volcano Laziale.
机译:研究了2011年发现的类石凝灰岩(Ricci pit,Agro Pontino,南拉齐奥,意大利),研究了其组成,成因和古地理意义。该凝灰岩是在拉齐奥南部的沿海盆地中首次出现的伍尔米时代的特菲拉层。根据其矿物学和同位素组成(Sr和Nd),它被确定为火山Laziale的远端特非拉沉积物,与阿尔巴诺6-7喷发相(“ Lapis Albanus”)有关,历史可追溯至41-36 ka BP。当Agro Pontino grab斗的中央部分仍由未解剖的平泻湖平原组成时,类固醇凝灰岩由经过重新加工并随后石蜡化的提弗拉组成。这项研究证实了该特菲拉层早已确立了其作为意大利中部地层标记的重要性,并表明其分布比先前所假设的要宽,尤其是在火山Laziale的东南部。

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