Titlebook: Geology and Landscapes of the Eastern Pyrenees; A Field Guide with E Marc Calvet,Magali Delmas,Bernard Laumonier Book 2022 Springer Nature

虛構的東西

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

激怒

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

Jocose

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

agglomerate

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

鐵塔等

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

FLUSH

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

Osmosis

Crumple

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

Nomadic

978-3-030-84265-9Springer Nature Switzerland AG 2022

Carcinoma