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Автор(ы):High L.R., Picard M.D.
Издание:Elsevier, 1973 г., 240 стр., ISBN: 0-444-41100-3
Язык(и)Английский
Developments in sedimentology. Vol 17. Sedimentary structures of ephemeral streams / Достижения в седиментологии. Том 17. Осадочные структуры кратковременных потоков

Ephemeral streams, dry washes, gullies, draws and arroyos are common names for a major element of Western landscapes. By definition ephemeral streams are characterized by short periods of flow, following local and intense rainfall, and alternating with long periods in which the channel is dry (Fig.] ,2).

Редактор(ы):Straaten L.M.J.U.
Издание:Elsevier, 1964 г., 480 стр.
Язык(и)Английский
Developments in sedimentology. Volume 1. Deltaic and shallow marine deposits / Достижения в седиментологии. Том 1. Дельтовые и мелководные морские отложения

The great contributions of CAYEUX (1941) have been a major factor in recognizing the environments in which sediments were deposited. However, I can certainly agree with BROUWER (1962) that Cayeux was too pessimistic in saying that it is uniquely by the analysis of ancient sediments that we can get to understand the conditions in marine basins of the past. It is quite possible that some of these ancient deposits were formed under conditions that no longer exist, but it seems likely that our failure to find analogies between past and present is due largely to the sparcity of studies in modern sedimentary basins. Compared to the thousands of geologists who are investigating ancient sediments there are only a handful of us who have been studying the Recent although we now have many new recruits. <...>

Автор(ы):Pollard L.D., Weaver C.
Издание:Elsevier, 1973 г., 221 стр., ISBN: 0-444-41043-0
Язык(и)Английский
Developments in sedimentology. Volume 15. The chemistry of clay minerals / Исследования в седиментологии. Том 15. Химия глинистых минералов

Clay minerals occur in all types of sediments and sedimentary rocks and are a common constituent of hydrothermal deposits. They are the most abundant minerals in sedimentary rocks perhaps comprising as much as 40% of the minerals in these rocks. Half or more of the clay minerals in the earth's crust are illites, followed, in order of relative abundance, by montmorillonite and mixed-layer illite-montmorillonite, chlorite and mixed-layer chlorite-montmorillonite, kaolinite and septachlorite, attapulgite and sepiolite. The clay minerals are fine-grained. They are built up of tetrahedrally (Si, A l , Fe3+) and octahedrally (Al, Fe3+, Fez+, Mg) coordinated cations organized to form either sheets or chains. All are hydrous. <...>

Редактор(ы):Konigshof P.
Издание:The Geological Society of London, 2009 г., 300 стр., ISBN: 978-1-86239-273-1
Язык(и)Английский
Devonian change: Case studies in palaeogeography and palaeoecology / Изменения в девоне: изучение примеров, палеогеография и палеоэкология

The Devonian was a critical period with respect to the diversification of early terrestrial ecosystems. The geotectonic setting was characterized by the switch from the post-Caledonian to the pre-Variscan situation. Plant life on land evolved from tiny tracheophytes to trees of considerable size in combination with a global increase in terrestrial biomass, and vertebrates started to conquer the land. Extensive shallow-marine areas and continental lowlands with a wide range of different habitats existed. These are preserved in a large number of basins all around the world. Climate change finally led from greenhouse to icehouse conditions towards the end of the Devonian. Rapid evolution of terrestrial ecosystems and climate change had a pronounced influence on sedimentation and biodiversity, not only in the terrestrial, but also in the marine realm. This volume contains case studies from Australia, China, Europe, South America and North America, and individual palaeoecosystems and their components have been investigated in different palaeogeographic settings that contribute to a much better understanding of the Devonian Period. This is a contribution to the IGCP 499 project on "Devonian land-sea interaction: evolution of ecosystems and climate”. <...>

Издание:PGS Publishing, Linden Park, 2005 г., 13 стр.
Язык(и)Английский
Dexing Porphyry Copper Deposits in Jiangxi, China

The Dexing porphyry copper field in Jiangxi, China, is defined by three porphyry copper deposits which are, from southeast to northwest, Fujiawu, Tongchang and Zhushahong respectively, and by the Guanmaoshan gold deposit which lies between Fujiawu and Tongchang. Technically, the field lies on the southeastern edge of the Jiangnan Anteclise, and is controlled by the NE-trending, deep-seated, Gandongbei fracture zone. The emplacement of the ore-bearing Fujiawu, Tongchang and Zhushahong granodiorite porphyry intrusions, dated at 184-172 Ma (Zhu et ah, 1983; Zhu et al9 1990), was also controlled by NW-trending structures. Mineralisation and alteration continued from 172 Ma to 100 Ma, and are characterised by symmetric zoning centred on the contacts between granodiorite porphyries and the enclosing country rocks of the Mesoproterozoic Shuangqiaoshan Group jrfryllites.

Редактор(ы):Matzner R.A.
Издание:CRC Press, 2001 г., 523 стр., ISBN: 0-8493-2891-8
Язык(и)Английский
Dictionary of geophysics, astrophysics, and astronomy / Геофизический, астрофизический и астрономический словарь

This work is the result of contributions from 52 active researchers in geophysics, astrophysics and astronomy. We have followed a philosophy of directness and simplicity, while still allowing contributors flexibility to expand in their own areas of expertise. They are cited in the contributors’ list, but I take this opportunity to thank the contributors for their efforts and their patience. The subject areas of this dictionary at the time of this writing are among the most active of the physical sciences. Astrophysics and astronomy are enjoying a new golden era, with remarkable observations in new wave bands (γ -rays, X-rays, infrared, radio) and in new fields: neutrino and (soon) gravitational wave astronomy.

Автор(ы):Taubenbaus H.
Издание:Safed, 1920 г., 72 стр.
Язык(и)Немецкий
Die Ammonecn der Kreideformation Palästinas und Syriens / Аммониты меловой формации Палестины и Сирии

Palästina, das schöne Land der Bibel, „dessen Gestein Eisen ist, und aus dessen Gebirge Kupfer gegraben wird“ (Dtn. 8,9), das Land, das seit Menschengedenken Ausgangspunkt großer Entwicklungen war, bietet im Gegensatz zu seiner * vielgestaltigen religiösen und politischen Geschichte geologisch ein sehr einfaches Bild, Dem Aufbau des Landes liegt ein Zwillingshorst aus harten Kreidekalkschichten zugrunde. Längs des Kiistenbruches läuft am Mittelmeer ein vorwiegend sandiger Streifen von Tertiär und Quartär <...>

Автор(ы):Schlosser M.
Издание:Munchen, 1881 г., 77 стр.
Язык(и)Немецкий
Die Fauna des Kelheimer Diceras-Kalkes. Erste Abtheilung: Vertebrata, Crustacea, Cephalopoda und Gastropoda / Фауна Кельхаймского известняка Дайцерас. Первое отделение: позвоночные, ракообразные, головоногие моллюски и брюхоногие моллюски

Schon seit langer Zeit hat der Kelheimer Jura die Aufmerksamkeit der Geologen auf sich gelenkt. Zwar hat die interessante Fauna des Platten - Kalkes durch Sömmering, v. Münster. H. v. Meyer, Andreas Wagner, Oppel u. A. eine treffliche Bearbeitung erfahren, dagegen sind unsere Kenntnisse von den Versteinerungen des Diceras-Kalkes noch so mangelhaft, dass es bisher nicht möglich war, den geologischen Horizont dieses Schichtencomplexes mit vollkommener Sicherheit festzustellen.

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