標(biāo)題: Titlebook: Geology and Landscapes of the Eastern Pyrenees; A Field Guide with E Marc Calvet,Magali Delmas,Bernard Laumonier Book 2022 Springer Nature [打印本頁] 作者: urinary-tract 時間: 2025-3-21 17:12
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作者: Flirtatious 時間: 2025-3-21 21:03 作者: FAWN 時間: 2025-3-22 04:12 作者: gait-cycle 時間: 2025-3-22 05:33
Functions of Several Variables,ow-gradient erosion surfaces of varying sizes and states of conservation, often in abrupt juxtaposition with (ii) a population of younger incisional landforms, themselves displaying evidence of successive stages of downcutting and drainage reorganisation such as dry valleys, wind gaps, mountain-flan作者: affluent 時間: 2025-3-22 12:46
Linear Spaces: New Spaces for Old,ean biogeographical regions meet, the species-rich eastern Pyrenees host a large proportion of endemic plant species. The different vegetation belts, which have undergone a long history of resource management and land-cover manipulation by human communities for the last 7500 years, are described and作者: ALIBI 時間: 2025-3-22 15:54 作者: ALIBI 時間: 2025-3-22 19:29 作者: 金哥占卜者 時間: 2025-3-22 23:08 作者: collagenase 時間: 2025-3-23 04:01 作者: antiquated 時間: 2025-3-23 07:43
2364-6497 level and climate-related changes over than same time period; (iii) geoheritage, i.e. educational vignettes of the flagship landscape units and typical geological sections of the study area. Written as a field 978-3-030-84265-9978-3-030-84266-6Series ISSN 2364-6497 Series E-ISSN 2364-6500 作者: 虛構(gòu)的東西 時間: 2025-3-23 10:52
Crustal Architecture of the Pyreneesence followed by collision in two successive stages during the late Cretaceous and Paleogene. The palaeogeography of the earlier Mesozoic topography (proto-Pyrenees) and of the main collisional orogen prevalent in mid Cenozoic time (syn-orogenic, or ancestral, Pyrenees) is sketched out. The chapter 作者: 激怒 時間: 2025-3-23 17:14
Basin Analysis: The Sedimentary Record of Orogenic Growth and Decaye Aquitaine Basin, and the population of post-Eocene extensional basins along the Mediterranean seaboard. The chronology and spatial distribution of conglomerate sequences, the rock-cooling record of basement outcrops in the mountain belt, and denudation in the foreland basins themselves in relation作者: Jocose 時間: 2025-3-23 19:36
Cenozoic Transformations of the Mountain Range: Evidence from Denudation Chronology and Landformsow-gradient erosion surfaces of varying sizes and states of conservation, often in abrupt juxtaposition with (ii) a population of younger incisional landforms, themselves displaying evidence of successive stages of downcutting and drainage reorganisation such as dry valleys, wind gaps, mountain-flan作者: agglomerate 時間: 2025-3-24 00:12
Present-Day Environmentsean biogeographical regions meet, the species-rich eastern Pyrenees host a large proportion of endemic plant species. The different vegetation belts, which have undergone a long history of resource management and land-cover manipulation by human communities for the last 7500 years, are described and作者: 鐵塔等 時間: 2025-3-24 04:42
Synthesis and Overviewd sedimentary confinement. Mountain-front fan systems became ubiquitous on both sides of the orogen during this time interval. The chapter delivers a comparative analysis of the depositional histories in the pro- and retro-foreland basins of the orogen. Explanations to a number of recorded features 作者: FLUSH 時間: 2025-3-24 08:37
Itinerary 5. Aspects of the North-Pyrenean Zone and its Foreland: Agly, Fenouillèdes, Razès, Pays de, their respective base levels, and the tectonic regimes that initially drove and subsequently interrupted their completion. Their respective ages and past connections with the Paleogene conglomerates of the Aquitaine foreland are discussed. Groundwater karst landforms in the thick Jurassic and Lowe作者: Osmosis 時間: 2025-3-24 12:23 作者: Crumple 時間: 2025-3-24 17:03
Itinerary 9. Tectonic, Palaeogeographic, and Landscape Evolution of the South-Vergent Nappe Structurt-tectonic evolution. Combining itineraries 5 and 9 (with components of Itinerary 4) overall provides a full cross-section of the orogenic wedge. The area covered here also hosts a number of previously unreported or poorly known landforms and deposits that hold important clues about landscape evolut作者: Nomadic 時間: 2025-3-24 21:34
978-3-030-84265-9Springer Nature Switzerland AG 2022作者: Carcinoma 時間: 2025-3-25 02:14 作者: 步履蹣跚 時間: 2025-3-25 05:34
https://doi.org/10.1007/978-3-030-84266-6Pyrenean Orogen; Denudation Chronology; Glacial Landscapes; Mountain Uplift; Neogene Tectonostratigraphy作者: angina-pectoris 時間: 2025-3-25 07:39 作者: 表主動 時間: 2025-3-25 14:59 作者: 引起痛苦 時間: 2025-3-25 17:26 作者: 溫室 時間: 2025-3-25 21:32 作者: 遺留之物 時間: 2025-3-26 00:37
Introduction to Coordinate Geometry,y also providing additional clues about palaeogeography and base-level changes. Constraints on the chronostratigraphy of the foreland sequences are usually provided by the fossil record and by magnetostratigraphy. Basin analysis helps to reconstruct the tectonic regime and succession of depositional作者: 疏遠天際 時間: 2025-3-26 05:05 作者: MULTI 時間: 2025-3-26 11:32
Linear Spaces: New Spaces for Old,odern Pyrenees form a major climatic barrier between western Europe and Iberia. This climatic asymmetry has prevailed for at least the entire duration of the Quaternary, and probably much longer. In the Aquitaine Basin, the climate is temperate oceanic, with mild winters and evenly distributed preci作者: 可行 時間: 2025-3-26 14:48 作者: 臆斷 時間: 2025-3-26 20:35 作者: 隼鷹 時間: 2025-3-26 23:15
https://doi.org/10.1007/978-3-642-28006-1s are examined successively along the southern, western and northern boundaries of the basin. Each site visited documents key successions of fault movements, continental clastic influx, marine sedimentation, or landscape change in the surrounding uplands as a result of widespread extensional tectoni作者: 退出可食用 時間: 2025-3-27 01:23 作者: 慌張 時間: 2025-3-27 05:45 作者: DEBT 時間: 2025-3-27 13:10 作者: 搖曳的微光 時間: 2025-3-27 13:56 作者: 表狀態(tài) 時間: 2025-3-27 21:43
Charles V. Pollack Jr.,Victoria G. Riese the sediment record contained in the more westerly basins of Cerdagne and Capcir, which exclusively display late Miocene stratigraphic sequences until now not encountered among the extensional basins of itineraries 1–6. Another highlight is the widespread population of erosion surfaces that either 作者: Gustatory 時間: 2025-3-28 01:58 作者: 熱情贊揚 時間: 2025-3-28 06:01 作者: 閃光你我 時間: 2025-3-28 07:24 作者: 流浪 時間: 2025-3-28 10:27
Differential Diagnosis of Fractureistocene glaciation among the surrounding massifs. Late Pleistocene and older glacial landforms and deposits are particularly well documented because sequences of moraines and glacifluvial terraces are well preserved across the Cerdagne Basin floor.作者: limber 時間: 2025-3-28 16:39
Itinerary 8. Elevated Ranges and Interior Basins of the Axial Zone: The Lower Cerdagne Basin and itsistocene glaciation among the surrounding massifs. Late Pleistocene and older glacial landforms and deposits are particularly well documented because sequences of moraines and glacifluvial terraces are well preserved across the Cerdagne Basin floor.作者: 手工藝品 時間: 2025-3-28 19:45
https://doi.org/10.1007/978-3-642-55600-5hods, and where their geodynamic and palaeoclimatic context can be reconstructed from a variety of environmental archives. Insights are also gained into the Pleistocene and Holocene evolution of the coastal plains, highlighting the recurrence of catastrophic flooding in the valleys.作者: ALLAY 時間: 2025-3-29 01:54
Itinerary 1. Where the Pyrenees Meet the Sea: Geomorphological Evolution of the Corbières Oroclinehods, and where their geodynamic and palaeoclimatic context can be reconstructed from a variety of environmental archives. Insights are also gained into the Pleistocene and Holocene evolution of the coastal plains, highlighting the recurrence of catastrophic flooding in the valleys.作者: 釘牢 時間: 2025-3-29 03:36
https://doi.org/10.1007/978-3-642-28006-1 Plain. At Perpignan, the Natural History Museum hosts a display of Pliocene vertebrate fossils from the region, although the majority of specimens are kept by the Natural History Museum in Paris and at the university of Lyon.作者: 詩集 時間: 2025-3-29 08:20
https://doi.org/10.1007/978-88-470-2859-3 autumn storms periodically generate major hydrological extremes as elsewhere in Roussillon, unlike adjacent areas summers are also rarely dry. These paroxysms have left scars in the landscape as well as in the collective memory of its residents.作者: 搖曳 時間: 2025-3-29 13:58 作者: 暴行 時間: 2025-3-29 17:20 作者: 條街道往前推 時間: 2025-3-29 23:41
Itinerary 4. The Vallespir Landscape: Scars of Deluge and Hydrological Disaster autumn storms periodically generate major hydrological extremes as elsewhere in Roussillon, unlike adjacent areas summers are also rarely dry. These paroxysms have left scars in the landscape as well as in the collective memory of its residents.作者: aspersion 時間: 2025-3-30 01:02
Itinerary 7. Elevated Ranges and Interior Basins of the Axial Zone: The Upper Cerdagne Basin, Capcird by its relative remoteness from the Aquitaine, Ebro and Mediterranean base levels. A third focus is on the impact of Pleistocene glaciation among the northern massifs. Quaternary glacial chrononology is particularly well documented because sequences of moraines and glacifluvial terraces are well preserved across the intermontane basin floors.作者: Adenocarcinoma 時間: 2025-3-30 07:28
2364-6497 geodynamics and landscape evolution of the Pyrenees in the l.This book provides a synthesis of the physiography and geodynamics of the entire Pyrenean orogen and its foreland basins, providing the "big picture" (structure of the orogen and chronology of its formation, overview of its post-orogenic e作者: ligature 時間: 2025-3-30 11:47 作者: 同音 時間: 2025-3-30 15:37 作者: 觀察 時間: 2025-3-30 19:45 作者: 個人長篇演說 時間: 2025-3-30 23:37 作者: Prophylaxis 時間: 2025-3-31 02:48
Synthesis and Overviewetween Europe and Iberia went through three successive states: the proto-Pyrenees, the ancestral Pyrenees, and the modern Pyrenees. Throughout this period, the mountain range changed in length, width, relief and elevation. The proto-Pyrenees began to emerge in the east, forming a mountain range that作者: poliosis 時間: 2025-3-31 08:14
Itinerary 1. Where the Pyrenees Meet the Sea: Geomorphological Evolution of the Corbières Orocline base-level changes during the Neogene by examining fault systems, sediment lithostratigraphy and provenance, and erosion surface vestiges crosscutting folds and structures of the North-Pyrenean and Sub-Pyrenean zones. Stops include sites where the planar land surfaces have been dated by various met
