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Выпуск 98
Издание:Economic geology, 2003 г., 13 стр.
Язык(и)Английский
Timing Constraints of Gold Mineralization along the Carlin Trend Utilizing Apatite Fission-Track, 40Ar/39Ar, and Apatite (U-Th)/He Methods

Apatite fission-track analysis is used to demonstrate that the timing of gold mineralization at the Carlin East and Betze-Post deposits is 37.3 ± 1.5 Ma, based on the weighted mean of measured fission-track ages, and 41.6 ± 1.6 Ma, based on the weighted mean of the ages of the oldest fission tracks retained. Regional measured apatite fission-track ages cluster between 28 and 41 Ma to the south of the Carlin East deposit whereas measured ages are greater than ~56 Ma to the north. The regional trend of the apatite fission-track ages and the pattern of gravity and magnetic anomalies suggest that the thermal center for gold mineralization along the Carlin trend was south of the Carlin East deposit, near the 37 Ma Welches Canyon stock. Modeling of apatite fission-track-age data on both sides of the Post fault indicates that the Little Boulder stock was approximately 35°C cooler at 40 Ma relative to similarly positioned samples in the Goldstrike stock. It is unclear whether this thermal history difference across the Post fault is due to post-40 Ma differential exhumation or differential heating across the fault at the time of gold mineralization. Comparison of apatite fission-track and whole-rock 40Ar/39Ar ages from altered dikes in the ore zone at Carlin East demonstrates that 40Ar/39Ar ages do not reflect the age of gold mineralization, whereas the apatite fission-track ages were completely reset at the time of hydrother-mal activity. (U-Th)/He ages are younger than the inferred mineralization age and may reflect weak hy-drothermal activity associated with Miocene volcanism.

Выпуск 192
Издание:Elsevier, 2002 г., 23 стр.
Язык(и)Английский
Timing of accretion and collisional deformation in the Central Asian Orogenic Belt: implications of granite geochronology in the Bayankhongor Ophiolite Zone

Growing evidence suggests that the mechanism of Palaeozoic continental growth in Central Asia was by subduction– accretion with punctuated collisions that produced ophiolitic sutures between accreted blocks. The Bayankhongor ophiolite is the largest ophiolite in Mongolia and possibly all of Central Asia, and is interpreted to mark the collisional suture between the Baidrag and Hangai continental blocks. New 207Pb/206Pb zircon evaporation ages for granite plutons and dykes that intrude the ophiolite and its neighbouring lithotectonic units suggest that the ophiolite was obducted at c. 540 Ma at the beginning of a collisional event that lasted until c. 450 Ma. The new data, combined with that of previous studies, indicate regional correlation of isotopic ages north-westward from Bayankhongor to southern Tuva. These data record oceanic crust formation at c. 570 Ma, followed by approximately 30 million years of subduction–accretion that culminated in obduction of ophiolites, collision related metamorphism, and magmatism in the period c. 540–450 Ma. Correlation of isotopic-age data for the ophiolites of western Mongolia and southern Tuva suggests that the ophiolites define a major collisional suture in the Central Asian Orogenic Belt (CAOB) that defines the southern and western margins of the Hangai continental block.

Том 47, Выпуск 4
Издание:Russian Geology and Geophysics, 2006 г., 7 стр., УДК: 551.24:48 (574)
Язык(и)Английский
Timing of collision of the Kokchetav massif with Stepnyak Island arc on the basis of conodonts and radiolarians from siliceous rocks of juxtaposed terranes of different geodynamic seetings

The siliceous rocks from structures of the junction zone of the Kokchetav massif and Stepnyak trough that occur in turbidites of the accretionary wedge, silica-volcanogenic sequence of the Stepnyak trough and syntectonic olistostrome were dated on the basis of findings of conodonts and radiolarians within the Middle-Upper Arenigian (conodont zones O. evae, B. navis—lower Par. originalis). This range of time is marked by a powerful tectonic rearrangement, involved with the rearrangement of the accretionary wedge and overriding of the Kokchetav massif upon the Stepnyak fore-arc trough.

Выпуск 96
Автор(ы):Jean S. Cline
Издание:Economic geology, 2001 г., 16 стр.
Язык(и)Английский
Timing of gold and arsenic sulfide mineral deposition at the Getchell Carlin-type gold deposit, North-Central Nevada

Pregold mineralization at the Getchell Carlin-type gold deposit includes quartz and base metal vein mineralization associated with intrusion of a Cretaceous granodiorite stock. The veins contain minor pyrite and trace chalcopyrite, arsenopyrite, galena, and sphalerite. The pyrite is moderately coarse and, in thin section, has high relief, is well polished, and is fractured and locally cemented by the gold ore assemblage. White micas are associated with veins near the granodiorite intrusion. Gold was not observed or detected by fire assay analyses of samples or electron microprobe analyses of pyrites. Microprobe analyses show that pregold pyrites have near-stoichiometric compositions. Variable, low arsenic is present in pyrite in samples overprinted by gold mineralization. Secondary ion mass spectrometry (SIMS) analyses detected trace gold in the coarse, near-stoichiomet-ric pyrite in overprinted samples. The pregold vein assemblage was fractured and cemented by gold ore-stage mineralization

Выпуск 44
Редактор(ы):De Baets K., Klug C., Korn D., Kruta I., Mapes R.H.
Издание:Springer, 2015 г., 614 стр., ISBN: 978-94-017-9632-3
Язык(и)Английский
Topics in geobiology. Volume 44. Ammonoid paleobiology: from macroevolution to paleogeography / Темы в геобиологии. Том 44. Палеобиология аммоноидов: от макроэволюции к палеогеографии

Ammonoids are the quintessential fossils, seemingly covering all the major themes of paleontology. Method and theory of stratigraphic correlation using fossils? Albert Oppel, whose concepts of zonation were explicated and applied by W. J. Arkell exhaustively in his monumental works on the Jurassic System, immediately spring to mind-works based virtually exclusively on the stratigraphic distributions of ammonoid species. Evolution? W. Waagen leaps to mind, applying the term “mutation” to his ammonoid lineages, and thus introducing the word to the scientific literature well before geneticists co-opted “mutation” for their own, starkly different, use. <...>

Издание:Springer, New York - London, 2011 г., 506 стр., ISBN: 978-90-481-9599-2
Язык(и)Английский
Topics in igneous petrology / Темы магматической петрологии

“Topics in Igneous Petrology: A Tribute to Professor Mihir K. Bose”, as the title appropriately suggests, is a Festschrift, ably edited by Professors Jyotisankar Ray, Gautam Sen and Dr. Biswajit Ghosh. It includes 18 scientific papers by 53 authors from around the globe. This Festschrift is indeed a welcome tribute, a true “festival of writing”, celebrating the life and works of the honoree, the admirable Professor Bose, by his students, colleagues and acquaintances. Unfortunately, Professor Bose passed away on October 1, 2009 before seeing these papers in print. The papers cover a broad range of topics and focus on igneous petrology that is bound to attract attentions of many igneous petrologist-geochemist, and certainly Professor Bose would have found himself drawn to many of these papers with utmost interest.

ТематикаПетрология
Автор(ы):Cheesman J., Huggett R.
Издание:Prentice-Hall Inc, 2002 г., 287 стр., ISBN: 0-582-41857-7
Язык(и)Английский
Topography and the environment / Топография и окружающая среда

Topography is at once a fundamental and a subtle environmental factor. It wields large and small influences over all other factors of the ecosphere -climate, water storage and movement, soils, animals and plants, and human activities. Several conspicuous topographic influences are well known. Most readers will be aware that a hike up a mountain is the climatic equivalent of a trek from a lower to a higher latitude. They will also be familiar with the stark climatic and botanical contrasts between northfacing and south-facing slopes in the European Alps. Subtle influences are not so well known but are equally significant.

Издание:1997 г., 3 стр.
Язык(и)Английский
Towards 2000 – The AusIMM mineral resources and ore reserves estimation seminars and the JORC reporting code / На пути к 2000 году – Семинары AusIMM по оценке минеральных ресурсов и запасов руды и кодекс отчетности JORC

The Australasian Institute of Mining and Metallurgy (The AusIMM) has been one of the principal organisations behind the JORC Code, which has been adopted by the Australian Stock Exchange and the Australian Securities commission as the standard for reporting mineral resources and ore reserves. This is now starting to be recognised as the international standard, with the UK, the USA and Canada all examining some form of the JORC Code for their resource and reserve reporting guidelines. The AusIMM has now further taken the initiative to produce a major volume covering all aspects of world’s best practice in Mineral Resource and Ore Reserves estimation. This prestigious volume will be published in the year 2000. <...>

Издание:Economic geology, 2016 г., 23 стр.
Язык(и)Английский
Trace element content of pyrite from the Kapai Slate, St. Ives Gold District, Western Australia / Содержание микроэлементов в пирите из сланца Капай, золотой район Сент-Айвз, Западная Австралия

The Kapai Slate is a continuous, pyrite-rich carbonaceous shale horizon within the St. Ives Au district that is spatially related to high-grade Au mineralization. In situ laser ablation-inductively coupled mass spectrometry (LA-ICPMS) trace element analyses, in situ sensitive high resolution ion microprobe, stable isotope (SHRIMPSI) S isotope analyses, and optical microscopy pyrite texture analyses were used to examine the different pyrite types in the Kapai Slate and Au deposits. These data were also used to confirm that the trace element signature of sedimentary pyrite can be preserved in rocks that underwent upper to mid-greenschist facies metamorphism and significant hydrothermal overprint. The data were further utilized to gain a more detailed understanding of the ocean conditions during deposition of the Kapai Slate and determine whether some of the Au and S in the St. Ives district could have been sourced from the Kapai Slate.

Редактор(ы):Miller W.
Издание:Elsevier, 2007 г., 636 стр.
Язык(и)Английский
Trace fossils. Concepts, problems, prospects

We have been describing and attempting to interpret trace fossils, more or less effectively, for over a century. One could point to several times in the history of paleontology or sedimentary geology when ichnology, as a separate discipline, appears to take shape for the first time. This is largely a matter of when the various early practitioners were active. I will leave it to the historians of our discipline to nail down all the exact dates, key figures and origins of ideas. A concise historical sketch can be found in the introduction to Ekdale et al. (1984). It is clear from this brief account, and from the longer essay by Osgood (1975) and especially the excellent historical chapters that follow, that the origins of ichnology are varied but that the discipline takes on its modern methodologic and conceptual aspects in the 1950s and 1960s. In anglophone countries, this development is usually associated with a ‘founder’ (Dolf Seilacher, signaled especially by a series of extremely influential articles: e.g., 1953, 1962, 1964, 1967a,b) and a ‘founding document’ (Ha¨ntzschel, 1962, 1975)—at least for invertebrate ichnology. Vertebrate and plant trace fossil researchers would tell the story a bit differently (see the essays that follow). But most of the central concepts and methods start to circulate and become widely applied or discussed at about this time.

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