The Geology of Iberia: A Geodynamic Approach: Volume 4: Cenozoic Basins
暫譯: 伊比利亞的地質：一種地動力學方法：第4卷：新生代盆地
Quesada, Cecilio, Oliveira, Jose Tomas
- 出版商: Springer
- 出版日期: 2019-06-17
- 售價: $6,600
- 貴賓價: 9.5 折 $6,270
- 語言: 英文
- 頁數: 184
- 裝訂: Hardcover - also called cloth, retail trade, or trade
- ISBN: 303011189X
- ISBN-13: 9783030111892
海外代購書籍(需單獨結帳)
相關主題
商品描述
Pursuing an innovative, global approach, this unique book provides an updated review of the geology of Iberia and its continental margins from a geodynamic perspective. Owing to its location close to successive plate margins, Iberia has played a pivotal role in the geodynamic evolution of the Gondwanan, Rheic, Pangea, Tethys and Eurasian plates over the last 600 Ma of Earth's history. The geological record starts with the amalgamation of Gondwana in the Neoproterozoic, which was succeeded by the rifting and spreading of the Rheic ocean; its demise, which led to the amalgamation of Pangea in the late Paleozoic; the rifting and spreading of several arms of the Neotethys ocean in the Mesozoic Era and their ongoing closure, which was responsible for the Alpine orogeny. The significant advances in the last 20 years have increasingly attracted international interest in exploring the geology of the Iberian Peninsula.
This volume focuses on the Cenozoic basins of the Iberian Geology and consequently the most recent sedimentary features in the Iberian Geology apart of the active ones. In this book, you will find a detailed explanation of the alpine foreland basins, the extension of the west Mediterranean as well as the latest magmatism in Iberia.
商品描述(中文翻譯)
追求創新且具全球視野的這本獨特書籍，從地動力學的角度提供了伊比利亞及其大陸邊緣地質的最新回顧。由於其位於接連的板塊邊緣附近，伊比利亞在過去六億年的地球歷史中，對於岡瓦納（Gondwana）、瑞克（Rheic）、盤古（Pangea）、特提斯（Tethys）和歐亞板塊的地動力演化扮演了關鍵角色。地質記錄始於新元古代的岡瓦納合併，隨後是瑞克海洋的裂解與擴張；其衰亡導致了晚古生代的盤古合併；在中生代期間，數個新特提斯海洋的分支裂解與擴張及其持續的閉合，造成了阿爾卑斯造山運動。過去20年來的重大進展，越來越吸引國際社會對伊比利亞半島地質的探索興趣。
本卷專注於伊比利亞地質的新生代盆地，因此涵蓋了伊比利亞地質中最新的沉積特徵，除了活躍的部分。在這本書中，您將找到有關阿爾卑斯前緣盆地、西地中海延伸以及伊比利亞最新岩漿活動的詳細解釋。
作者簡介
José Tomás Oliveira holds a Ph.D. and Agregação (Portuguese postdoctoral degree). He is a geologist and is currently collaborating at Laboratorio Nacional de Energia e Geologia, former Geological Survey of Portugal, where he acted also as Head of the Geology and Mineral Resources departments. As a survey geologist, his main activities have focused on regional geological mapping in Portugal and Mozambique, with a particular interest in stratigraphy, clastic sedimentology and basin analysis. He has been an Invited Professor at universities in Portugal and Angola, author and editor of several geological maps, and was co-editor of the recently published Geological Map of Portugal and Spain, 2015, scale 1:1,000,000.
作者簡介(中文翻譯)
塞西利奧·奎薩達（Cecilio Quesada）的職業生涯主要在西班牙地質礦業研究所（Instituto Geológico Minero de España）工作，直到2013年退休。他目前是馬德里康普頓斯大學（Universidad Complutense）地質科學院的名譽教授，並曾暫時擔任副教授。作為一名「調查人員」，他的研究興趣包括地質製圖、區域地質學、構造學和地質年代學，主要集中在全球背景下的瓦里斯坎造山運動（Variscan orogen）。自1979年以來，他參與了十個國際地質科學計畫（IGCP），目前參與的計畫是648號：超大陸循環與全球地球動力學。
何塞·托馬斯·奧利維拉（José Tomás Oliveira）擁有博士學位及葡萄牙的後博士學位Agregação。他是一名地質學家，目前在葡萄牙前地質調查局的國家能源與地質實驗室（Laboratorio Nacional de Energia e Geologia）合作，並曾擔任地質與礦產資源部門的負責人。作為一名調查地質學家，他的主要活動集中在葡萄牙和莫桑比克的區域地質製圖，特別關注地層學、碎屑沉積學和盆地分析。他曾在葡萄牙和安哥拉的多所大學擔任受邀教授，並是幾幅地質圖的作者和編輯，還是最近出版的《葡萄牙和西班牙地質圖》（Geological Map of Portugal and Spain, 2015，比例尺1:1,000,000）的共同編輯。
