干旱区生态环境知识资源中心(Arid): New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain

Arid

DOI	10.1016/j.earscirev.2018.11.008
	New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain
	Lopez-Gomez, Jose 1; Martin-Gonzalez, Fidel 1,2; Heredia, Nemesio ; de la Horra, Raul 3,4; Barrenecheaa, Jose F.1,5; Cadenas, Patricia ; Juncal, Manuel 7; Diez, Jose B.7; Borruel-Abadia, Violeta 1,8; Pedreira, David 6; Garcia-Sansegundo, Joaquin 6; Farias, Pedro 6; Gale, Carlos ; Lago, Marceliano 9; Ubide, Teresa 10; Fernandez-Viejo, Gabriela 6; Gand, Georges 11
通讯作者	Lopez-Gomez, Jose
来源期刊	EARTH-SCIENCE REVIEWS
ISSN	0012-8252
EISSN	1872-6828
出版年	2019
卷号	188 页码:249-271
英文摘要	The Pyrenean-Cantabrian Orogen arose through the collision of the Iberian and Eurasian plates, mostly in Cenozoic times. This orogen comprises two main mountain ranges, the Pyrenees to the east, and the Cantabrian Mountains to the west. To date, the early Alpine tectono-sedimentary phases preserved in the Cantabrian Mountains, of Permian and Triassic age, have been considered independently from the same phases in neighbouring basins of SW Europe, and even from the eastern part of the same orogeny (the Pyrenean orogeny). In consequence, the beginning of the Alpine cycle in the Cantabrian Mountains has been interpreted within a specific geodynamic context, far from the general evolutionary phases of the western Peri-Tethys basins. Through detailed field work, including geological mapping, sedimentology, lithostratigraphy and petrology of volcanic rocks, and new palaeontological data, here we define several new lithostratigraphical formations and five new tectono-sedimentary cycles (TS I-V) for the initial phases of evolution of the Mesozoic Basque Cantabrian Basin, interrupted by periods of tectonic stability. To complete this information, we include data from an onshore borehole (Villabona Mine) and two offshore boreholes constrained by 2D reflection seismic profiles acquired in the North Iberian continental platform. The main tectono-sedimentary cycles, related to the deposition of five major identified lithostratigraphic units, can be described as follows: TS I (late Gzelian-early Asselian), relating to the late Variscan deformation and preserved in a single outcrop in all the Cantabrian Mountains (San Tirso Formation). This formation is constituted by medium-distal alluvial fan deposits in which humid intervals predominate, forming some thin coal beds. TS II (Asselian-Sakmarian), a post-Variscan extensional phase with associated calc-alkaline magmatism, represented by profuse volcanic and volcanosedimentary intercalations in the early Permian sedimentary basins (Acebal Formation) and small plutons in surrounding areas. TS III (Kungurian), or reactivation of the post-Variscan extension leading to alluvial and lacustrine carbonate sedimentation in arid climate conditions, which do not change during the rest of the Permian and Triassic periods (Sotres Formation). A generalized karstification in the basin represents the end of Permian deposition, followed by an interruption in sedimentation longer than 30 Myr. The Permian tectono-sedimentary cycles (TS II and TS III) are contemporary with Variscan belt collapse and the basins are controlled by extensional reactivation of NE-SW and E-W Variscan structures, and NW-SE late Variscan structures. TS IV (late Anisian-middle Carnian), renewed sedimentation in more extensive basins, precursors of the great Mesozoic Basque-Cantabrian Basin. This cycle is represented by fluvial deposits (Cicera Formation, or Buntsandstein facies), which are interrupted by the first Mesozoic marine ingression (Rueda Formation, or Muschelkalk facies). TS V (Norian-Rhaetian), or shallow marine carbonate deposits (Transicion Formation) related to increasingly compartmentalized sub-basins, controlled by normal faults. This final TS is broadly connected with different basins of the western Peri-Tethys domain. The identification of units TS I-V in the Cantabrian Mountains along with the volcanic character of TS H, all indicate the development of a common post-Variscan to early Alpine tectono-sedimentary evolution for the whole Pyrenean-Cantabrian realm.
英文关键词	Cantabrian Mountains Pyrenees Pyrenean-Cantabrian orogen Alpine cycle Permian-Triassic Post-variscan tectonics
类型	Review
语种	英语
国家	Spain ; Australia ; France
开放获取类型	Green Accepted, Green Submitted
收录类别	SCI-E
WOS记录号	WOS:000463462500012
WOS关键词	HYPEREXTENDED RIFT SYSTEMS ; SEISMIC-REFLECTION ; IBERIAN PENINSULA ; ASTURIAN BASIN ; VARISCAN ; BAY ; TECTONICS ; BISCAY ; DEFORMATION ; EUROPA
WOS类目	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/2XILL650/215105
作者单位	1.Univ Complutense Madrid, CSIC UCM, Inst Geociencias, C Doctor Severo Ochoa 7,4, E-28040 Madrid, Spain; 2.Univ Rey Juan Carlos, Area Geol ESCET, C Tulipan S-N, Madrid 28933, Spain; 3.IGME, C Matemdtico Pedrayes 25, Oviedo E33005, Spain; 4.Univ Complutense, Fac Ciencias Geol, Dept Geodinam Estratig & Paleontol, C Jose Antonio Novais 2, E-28040 Madrid, Spain; 5.Univ Complutense, Fac Geol, Dept Mineral & Petr, C Jose Antonio Novais 2, E-28040 Madrid, Spain; 6.Univ Oviedo, Dept Geol, C Jesus Arias Velasco S-N, E-33005 Oviedo, Spain; 7.Univ Vigo, Fac Ciencias Mar, Dept Xeociencias Marinas & OT, Campus Lagoas Marcosende, Vigo 36310, Spain; 8.IGME, C Rios Rosas 23, Madrid 28003, Spain; 9.Univ Zaragoza, C Pedro Cerbuna 12, E-50009 Zaragoza, Spain; 10.Univ Queensland, Sch Earth & Environm Sci, Steele Building, Brisbane, Qld 4072, Australia; 11.Univ Bourgogne, Lab Biogeosci UMR CNRS UB 6282, 6 Bd Gabriel, F-21000 Dijon, France
推荐引用方式 GB/T 7714	Lopez-Gomez, Jose,Martin-Gonzalez, Fidel,Heredia, Nemesio,et al. New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain[J],2019,188:249-271.
APA	Lopez-Gomez, Jose.,Martin-Gonzalez, Fidel.,Heredia, Nemesio.,de la Horra, Raul.,Barrenecheaa, Jose F..,...&Gand, Georges.(2019).New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain.EARTH-SCIENCE REVIEWS,188,249-271.
MLA	Lopez-Gomez, Jose,et al."New lithostratigraphy for the Cantabrian Mountains: A common tectono-stratigraphic evolution for the onset of the Alpine cycle in the W Pyrenean realm, N Spain".EARTH-SCIENCE REVIEWS 188(2019):249-271.