標(biāo)題: Titlebook: Anatomy of an Orogen: The Apennines and Adjacent Mediterranean Basins; Gian Battista Vai,I. Peter Martini Book 2001 Springer Science+Busin [打印本頁(yè)] 作者: Coenzyme 時(shí)間: 2025-3-21 19:17
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作者: 有發(fā)明天才 時(shí)間: 2025-3-21 20:46 作者: Herd-Immunity 時(shí)間: 2025-3-22 01:05
Book 2001onal audience. However, sufficient detailsand in-depth analyses of the various complex settings have beenpresented to make this material useful to professional scholars and tostudents of senior university courses.作者: 否認(rèn) 時(shí)間: 2025-3-22 06:24 作者: 蚊帳 時(shí)間: 2025-3-22 12:35 作者: Headstrong 時(shí)間: 2025-3-22 15:36
Tertiary silicoclastic turbidite systems of the Northern Apennines,deep units have not always been documented in the same accurate way as the MA and the overall stratigraphie scheme is still to be refined. Within these limitations, this contribution aims at presenting a review of the stratigraphy, basin geometry and tectonic signature of the Tertiary foredeep depos作者: 壁畫 時(shí)間: 2025-3-22 19:01 作者: GENRE 時(shí)間: 2025-3-23 00:10
Anatomy of an Orogen: The Apennines and Adjacent Mediterranean Basins978-94-015-9829-3作者: humectant 時(shí)間: 2025-3-23 04:23 作者: exquisite 時(shí)間: 2025-3-23 08:37 作者: 怒目而視 時(shí)間: 2025-3-23 12:34
Deep structure from seismic tomography,mechanisms has been ongoing for many years. One of the reasons for this has been the poor knowledge of the crust and upper mantle structure, and the lack of precise information on the occurrence of intermediate and deep earthquakes beneath the Italian peninsula. In this chapter we describe the advan作者: 上坡 時(shí)間: 2025-3-23 15:01 作者: geometrician 時(shí)間: 2025-3-23 19:36 作者: Water-Brash 時(shí)間: 2025-3-24 00:30
Volcanism in the Southern Apennines and Sicily,any to Basilicata, which includes the Alban Hills south of Rome, Vesuvius, the Campi Flegrei caldera, and the isolated Mt Vulture volcano; (2) the Tyrrhenian oceanic basin; (3) the Aeolian island arc; (4) eastern Sicily with Etna and the Hyblean plateau; and (5) the submarine and emerged volcanoes i作者: CRAFT 時(shí)間: 2025-3-24 05:10
Basement and early (pre-Alpine) history,rly expressed by the transition from the Quaternary SE Tyrrhenian oceanic crust to the possible late Proterozoic age of the Panafrican consolidated NE Apulian continental crust (Vai, 1994), which occurs in over a distance of only 170 km. Between the two, several other crustal provinces are found in 作者: FER 時(shí)間: 2025-3-24 09:09
Ophiolites, Ligurides and the tectonic evolution from spreading to convergence of a Mesozoic Westerde unique records for reconstructing the opening, evolution and closure of the portion of Western Tethys that separated the European-Iberia plates to the NW from the Africa-Adria plates to the SE (Abbate .., 1970, 1980, 1986; Principi and Treves, 1984). They are present all along the Alps and the Ap作者: Lucubrate 時(shí)間: 2025-3-24 11:37 作者: essential-fats 時(shí)間: 2025-3-24 17:55 作者: 背信 時(shí)間: 2025-3-24 20:26
Inner Northern Apennines,e and on the Tuscan metamorphic complex (Boccaletti .., 1971; Alvarez .., 1974; Kligfield, 1979). The ophiolite-bearing Ligurides derived from the southern extension of the Ligurian—Piedmont ocean, from which similar mafic components of the Western Alps also derive (Fig. 14.1). The Tuscan units deri作者: AMITY 時(shí)間: 2025-3-25 00:49
Outer Northern Apennines,nding through Romagna and Umbria—Marche to northern Latium. From the SW to the NE, it is situated between the inner Northern Apennines and the Po Plain—Adriatic foreland. To the S, the volcanic products of the Roman magmatic province cover it, while to the SE it is bounded by the Latium—Abruzzi carb作者: 仔細(xì)檢查 時(shí)間: 2025-3-25 03:59 作者: Servile 時(shí)間: 2025-3-25 07:34
Calabria-Peloritani terrane and northern Ionian Sea,ane and the northern (N) Ionian Sea. A general introduction to the study area is followed by a brief overview of past interpretations, a description of its main tectono-stratigraphic units, and a new interpretation of its evolution in terms of terrane analysis and accretion history. The term Calabri作者: CLAN 時(shí)間: 2025-3-25 13:15 作者: 事情 時(shí)間: 2025-3-25 18:15 作者: 呼吸 時(shí)間: 2025-3-25 22:34 作者: Prologue 時(shí)間: 2025-3-26 01:12
https://doi.org/10.1007/978-1-4615-0921-9me of these terms, such as argille scagliose and olistostrome, have been applied to mélanges in other mountain chains, even while Apennine geologists continued to debate whether local examples resulted from tectonic or gravitational processes.作者: 推延 時(shí)間: 2025-3-26 07:15 作者: 騎師 時(shí)間: 2025-3-26 11:17 作者: 他一致 時(shí)間: 2025-3-26 15:37
https://doi.org/10.1007/978-1-4615-0921-9ath the Quaternary deposits of the Po Plain; that is (1) the N-facing Northern Apennines front, (2) the S-facing Southern Alps front and (3) the Adriatic-Po Plain foreland in between. The third section discusses possible interpretations and implications.作者: violate 時(shí)間: 2025-3-26 17:44
DP System Initial Testing Regime,a-Peloritani Arc, traditionally found in the literature, is discontinued because it refers to the present-day morphological curvature of the terrane in map view, but it is confusing if geologically defined.作者: 縱欲 時(shí)間: 2025-3-26 22:48
Geomorphologic setting,t a relatively fast rate (about 2500 m/Ma or 2.5 mm/a; Po Plain). Active tectonism renders this area prone to geological hazards such as those associated with volcanism, faulting and earthquakes, and slope instability.作者: 時(shí)間等 時(shí)間: 2025-3-27 05:09 作者: originality 時(shí)間: 2025-3-27 08:30 作者: 騷擾 時(shí)間: 2025-3-27 11:28 作者: Formidable 時(shí)間: 2025-3-27 14:54
Population Models With Constant Rates,ynamic context of Italian magmatism is discussed in much detail by Serri ... (this vol., Ch. 8), only brief summaries of the various recent hypotheses regarding the tectonic settings of these volcanoes will be given here.作者: 碳水化合物 時(shí)間: 2025-3-27 19:32
Strategies for Investment in Optionsits of the foreland consist of Mesozoic—Cenozoic carbonates up to 10 km thick (Burollet .., 1978; Patacca .., 1979; Bianchi .., 1989; Mostardini and Merlini, 1988), whereas the oceanic Ionian crust underlies thin Mesozoic—Cenozoic, deep-sea to oceanic sediments (Finetti .., 1996).作者: 他很靈活 時(shí)間: 2025-3-28 00:37
Deep structure from seismic tomography,ological tools, exploiting this huge dataset, have helped to unravel the complex structure of the lithosphere—asthenosphere system of the Mediterranean, and, thus, have contributed to a better understanding of the geodynamic evolution of the region.作者: MEAN 時(shí)間: 2025-3-28 06:05 作者: 彎曲的人 時(shí)間: 2025-3-28 09:06
,The Apenninic—Maghrebian orogen in southern Italy, Sicily and adjacent areas,its of the foreland consist of Mesozoic—Cenozoic carbonates up to 10 km thick (Burollet .., 1978; Patacca .., 1979; Bianchi .., 1989; Mostardini and Merlini, 1988), whereas the oceanic Ionian crust underlies thin Mesozoic—Cenozoic, deep-sea to oceanic sediments (Finetti .., 1996).作者: 施加 時(shí)間: 2025-3-28 13:07
world. The Apennines are the place from which Steno(1669) first stated the principles of geology. The Apennines alsorepresent amongst others, the finding/testing sites of processes andproducts like volcanic eruptions, earthquakes, olistostromes andmélanges (argille scagliose), salinity crisis, geoth作者: Atheroma 時(shí)間: 2025-3-28 14:56
Central Bank and Government Cooperate with the North African Maghrebian chain on the other side. It resulted from the interplay of various microplates in the oblique collisional belt between the African and Eurasian plates during Tertiary and Quaternary time.作者: seruting 時(shí)間: 2025-3-28 19:07 作者: 刺耳 時(shí)間: 2025-3-28 23:24 作者: 人充滿活力 時(shí)間: 2025-3-29 05:20 作者: Fretful 時(shí)間: 2025-3-29 08:29 作者: 保全 時(shí)間: 2025-3-29 12:01 作者: conduct 時(shí)間: 2025-3-29 15:39 作者: Fester 時(shí)間: 2025-3-29 21:05
Ophiolites, Ligurides and the tectonic evolution from spreading to convergence of a Mesozoic Westerthe NW from the Africa-Adria plates to the SE (Abbate .., 1970, 1980, 1986; Principi and Treves, 1984). They are present all along the Alps and the Apennines down to Calabria, except for central Italy. This chapter deals with the Northern Apennines, where these successions are well exposed and studied.作者: Canyon 時(shí)間: 2025-3-30 02:54 作者: 一起 時(shí)間: 2025-3-30 07:36
Outer Northern Apennines,n—Adriatic foreland. To the S, the volcanic products of the Roman magmatic province cover it, while to the SE it is bounded by the Latium—Abruzzi carbonate platform. As for the Alps—ONA boundary the reader is referred to Castellarin (this vol., Ch. 13).作者: 帶傷害 時(shí)間: 2025-3-30 10:12 作者: DEI 時(shí)間: 2025-3-30 15:45 作者: Certainty 時(shí)間: 2025-3-30 19:57 作者: 津貼 時(shí)間: 2025-3-30 22:08 作者: 拔出 時(shí)間: 2025-3-31 03:32
http://image.papertrans.cn/a/image/156960.jpg作者: 駁船 時(shí)間: 2025-3-31 06:51
https://doi.org/10.1007/978-3-642-18228-0The objective of this chapter is to provide a guide to what this book contains, what major conclusions the various contributors have proposed, and thus aid in the understanding of the geology of the Apennines (Fig. 2.1). To this purpose, the chapters of this book are reviewed, summarized with major points highlighted, compared and contrasted.作者: Baffle 時(shí)間: 2025-3-31 10:39
https://doi.org/10.1007/978-3-642-18228-0Deep-seated features of the Earth’s crust can be identified and characterized by the velocities or by the reflectivity of the transmitted seismic waves generated from artificial sources near the surface and recorded by seismographs distributed along profiles or fans.作者: 縫紉 時(shí)間: 2025-3-31 14:00 作者: 使絕緣 時(shí)間: 2025-3-31 17:58 作者: impaction 時(shí)間: 2025-4-1 01:36 作者: SLAG 時(shí)間: 2025-4-1 04:20
Magnetic and gravity analysis of Italy,The objective of this chapter is to analyse available magnetic and gravimetric data to better understand the structure of the Apennines and adjacent marine basins (Figs 6.1, 6.2).作者: Callus 時(shí)間: 2025-4-1 06:57 作者: 發(fā)芽 時(shí)間: 2025-4-1 12:48
Longevity and Dynamic Mortality,rly expressed by the transition from the Quaternary SE Tyrrhenian oceanic crust to the possible late Proterozoic age of the Panafrican consolidated NE Apulian continental crust (Vai, 1994), which occurs in over a distance of only 170 km. Between the two, several other crustal provinces are found in this relatively small area.作者: Matrimony 時(shí)間: 2025-4-1 16:24
