Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.3301/IJG.2019.27 |
The Carboniferous-mid Permian successions of the Northern Apennines: new data from the Pisani Mts. inlier (Tuscany, Italy) | |
Marini, Federico; Pandeli, Enrico; Tongiorgi, Marco; Pecchioni, Elena; Orti, Letizia | |
通讯作者 | Pandeli, E |
来源期刊 | ITALIAN JOURNAL OF GEOSCIENCES |
ISSN | 2038-1719 |
EISSN | 2038-1727 |
出版年 | 2020 |
卷号 | 139期号:2页码:212-232 |
英文摘要 | This paper updates and partially modifies the knowledge of the geological-palaeoenvironmental and geodynamic framework of the Tuscan segment of the Variscan Chain during Permian times. Particularly, it adds new data on the contact between the upper Carboniferous-lower Permian San Lorenzo schist (SLs) and the mid-Permian Asciano breccia and conglomerate (Abc) clastic formations in the Pisani Mts. metamorphic inlier which represents one of the key outcrops for the study of the upper Paleozoic sequences in the Northern Apennines. Their sharp unconformable contact is well documented in the literature at map and outcrop scale and was ascribed to the Saalian phase of the Variscan orogeny that would have occurred in correspondence of a climatic change from equatorial to semi-arid tropical conditions. New geological investigations on the SLs and Abc led to the finding of a continuous stratigraphic section in the Pian della Conserva locality (northwestern Pisani Mts.) where the organic matter-rich SLs conformably passes upwards to the reddish immature, mainly coarse-grained deposits of Abc represents a decametric transition zone. The section was studied in detail from a lithological-sedimentological point of view and sampled for petrographic, mineralogic and chemical studies. The data show that the passage from SLs to Abc represents a main change from an equatorial, wet fluvial-lacustrine environment to a well-drained, alluvial fan system in a monsoon-like climate. This event can be related to the reactivation of the previous late Carboniferous-early Permian shear zones during mid-Permian times. Such reactivation produced morpho-tectonic highs subjected to a rapid erosion and the formation of unconformities, whereas the presence of a few residual fluvial plain areas, characterized by dysoxic conditions, is documented by the gradual passage between SLs and Abc in the Pian della Conserva section. In addition, the presence of a metavolcanoclastic or metaepiclastic layer was also recognized in the uppermost part of the SLs and it represents the first evidence of a late Carboniferous-early Permian volcanic event in the Northern Apennines. |
英文关键词 | Pisani Mts. late Paleozoic stratigraphy petrography geochemistry palaeogeography Tuscany |
类型 | Article |
语种 | 英语 |
开放获取类型 | Green Submitted |
收录类别 | SCI-E |
WOS记录号 | WOS:000537714500003 |
WOS关键词 | MONTICIANO-ROCCASTRADA RIDGE ; MOUNTAINS TUSCANY ; SOUTHERN TUSCANY ; EASTERN LOMBARDY ; SHEAR ZONE ; EVOLUTION ; VARISCAN ; VERRUCANO ; WESTERN ; ALPINE |
WOS类目 | Geology ; Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/324630 |
作者单位 | [Marini, Federico; Pandeli, Enrico; Pecchioni, Elena; Orti, Letizia] Univ Firenze, Dept Earth Sci, Via G La Pira 4, I-50121 Florence, Italy; [Pandeli, Enrico] IGG CNR Pisa, Florence Sect, Geosci & Earth Resources Inst, Via G La Pira 4, I-50121 Florence, Italy; [Tongiorgi, Marco] Univ Pisa, Dept Earth Sci, Museum Nat Hist, Via Roma 79, I-56011 Pisa, Italy |
推荐引用方式 GB/T 7714 | Marini, Federico,Pandeli, Enrico,Tongiorgi, Marco,et al. The Carboniferous-mid Permian successions of the Northern Apennines: new data from the Pisani Mts. inlier (Tuscany, Italy)[J],2020,139(2):212-232. |
APA | Marini, Federico,Pandeli, Enrico,Tongiorgi, Marco,Pecchioni, Elena,&Orti, Letizia.(2020).The Carboniferous-mid Permian successions of the Northern Apennines: new data from the Pisani Mts. inlier (Tuscany, Italy).ITALIAN JOURNAL OF GEOSCIENCES,139(2),212-232. |
MLA | Marini, Federico,et al."The Carboniferous-mid Permian successions of the Northern Apennines: new data from the Pisani Mts. inlier (Tuscany, Italy)".ITALIAN JOURNAL OF GEOSCIENCES 139.2(2020):212-232. |
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