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1.
ALLAN MILLS 《Geology Today》1994,10(4):157-159
'Since this matter remains in dispute and causes much dissention amongst miners, I consider it ought to be examined on its own merits.'– Georgius Agricola . 相似文献
2.
Sophie GODIN-BEEKMANN Irina PETROPAVLOSKIKH Stefan REIS Paul NEWMAN Wolfgang STEINBRECHT Markus REX Michelle L. SANTEE Richard S. ECKMAN Xiangdong ZHENG Matthew B. TULLY David S. STEVENSON Paul YOUNG John PYLE Mark WEBER Johanna TAMMINEN Gina MILLS Alkis F. BAIS Clare HEAVISIDE Christos ZEREFOS 《大气科学进展》2017,34(3):283-288
<正>1.Overview The 2016 Quadrennial Ozone Symposium(QOS-2016)was held on 4–9 September 2016 in Edinburgh,UK.The Symposium was organized by the International Ozone Commission(IO3C),the NERC Centre for EcologyHydrology and the University of Edinburgh,and was co-sponsored by the International Union of Geodesy and Geophysics,the International Association of Meteorology and Atmospheric 相似文献
3.
Sophie GODIN-BEEKMANN Irina PETROPAVLOSKIKH Stefan REIS Paul NEWMAN Wolfgang STEINBRECHT Markus REX Michelle L. SANTEE Richard S. ECKMAN Xiangdong ZHENG Matthew B. TULLY David S. STEVENSON Paul YOUNG John PYLE Mark WEBER Johanna TAMMINEN Gina MILLS Alkiviadis F. BAIS Clare HEAVISIDE Christos ZEREFOS 《大气科学进展》2018,35(3):368-369
4.
Two picrite flows from the SW rift zone of Mauna Loa containxenoliths of dunite, harzburgite, lherzolite, plagioclase-bearinglherzolite and harzburgite, troctolite, gabbro, olivine gabbro,and gabbronorite. Textures and olivine compositions precludea mantle source for the xenoliths, and rare earth element concentrationsof xenoliths and clinopyroxene indicate that the xenolith sourceis not old oceanic crust, but rather a Hawaiian, tholeiitic-stagemagma. Pyroxene compositions, phase assemblages and texturalrelationships in xenoliths indicate at least two different crystallizationsequences. Calculations using the pMELTS algorithm show thatthe two sequences result from crystallization of primitive MaunaLoa magmas at 6 kbar and 2 kbar. Independent calculations ofolivine Ni–Fo compositional variability in the plagioclase-bearingxenoliths over these crystallization sequences are consistentwith observed olivine compositional variability. Two parentsof similar bulk composition, but which vary in Ni content, arenecessary to explain the olivine compositional variability inthe dunite and plagioclase-free peridotitic xenoliths. Xenolithsprobably crystallized in a small magma storage area beneaththe rift zone, rather than the large sub-caldera magma reservoir.Primitive, picritic magmas are introduced to isolated rift zonestorage areas during periods of high magma flux. Subsequenteruptions reoccupy these areas, and entrain and transport xenolithsto the surface. KEY WORDS: xenolith; Hawaii; volcano plumbing; mineral composition; picrite 相似文献
5.
Abstract The Dras 1 Volcanic Formation of the Ladakh Himalaya, India, represents the eastern, upper crustal equivalent of the lower crustal gabbros and mantle peridotites of the Kohistan Arc exposed in Pakistan. Together these form a Cretaceous intraoceanic arc now located within the Indus Suture zone between India and Eurasia. During the Late Cretaceous, the Dras–Kohistan Arc, which was located above a north-dipping subduction zone, collided with the south-facing active margin of Eurasia, resulting in a switch from oceanic to continental arc volcanism. In the present study we analyzed samples from the pre-collisional Dras 1 Volcanic Formation and the postcollisional Kardung Volcanic Formation for a suite of trace elements and Nd isotopes. The Kardung Volcanic Formation shows more pronounced light rare earth element enrichment, higher Th/La and lower ɛNd values compared with the Dras 1 Volcanic Formation. These differences are consistent with an increase in the reworking of the continental crust by sediment subduction through the arc after collision. As little as 20% of the Nd in the Dras 1 Volcanic Formation might be provided by sources such as the Karakoram, while approximately 45% of the Nd in the Kardung Volcanic Formation is from this source. However, even before collision, the Dras–Kohistan Arc shows geochemical evidence for more continental sediment contamination than is seen in modern western Pacific arcs, implying its relative proximity to the Eurasian landmass. Comparison of the lava chemistry in the Dras–Kohistan Arc with that in the forearc turbidites suggests that these sediments are partially postcollisional, Jurutze Formation and not all pre-collisional Nindam Formation. Thus, the Dras–Eurasia collision can be dated as Turonian–Santonian (83.5–93.5 Ma), older than it was previously considered to be, but consistent with radiometric ages from Kohistan. 相似文献
6.
BY STEPHANIE C. MILLS STEFAN W. GRAB SIMON J. CARR 《Geografiska Annaler: Series A, Physical Geography》2009,91(2):121-140
Considerable Quaternary environmental reconstruction for the high Drakensberg is based on geomorphological and sedimentological work undertaken along the northern aspects of the Sekhokong mountain range of eastern Lesotho. Given that no previous investigations have focused on the southern aspects, this paper documents the observed geomorphology and provides a more complete palaeo-environmental picture for this range. Data on the morphology, sedimentology and micromorphology for two linear debris ridges are presented. It is demonstrated that the two ridges are most likely moraines originating from a small niche glacier. The combined use of macro- and micro-scale sedimentology is proven to be an essential tool in ascribing a glacial process origin for the landforms, given the complex depositional history they have undergone. AMS ages obtained from the deposits (14 700 cal. yrs bp and 19 350 cal. yrs bp ) places these in the time-scale of the Last Glacial Maximum. The study demonstrates rather contrasting aspect-controlled palaegeomorphological environments along the Sekhokong range, which is also reflected in the dissimilar contemporary biophysical micro-environments. It is suggested that the south-facing slopes were dominated by glacial processes during the Last Glacial Maximum (LGM), as is evident from the moraines, while the proposition for previously described north-facing glacial cirques is rejected based on the absence of erosional/depositional evidence and greater insolation received on these warmerequator-facing slopes. Rather, we propose that the observed north-facing hollows are a product of a multitude of geomorphic processes spanning several tens to hundreds of thousands of years. 相似文献
7.
This paper provides an assessment of the conceptual basis of community forestry from around the world, based on case studies presented in the literature, mainly over the last decade. More than 400 documents were examined for this comprehensive qualitative meta-study (meta-theory, meta-analysis, meta-method, and meta-synthesis) of community forestry. An overall conclusion is offered regarding the extent to which community forestry can be adapted to foster practices that enhance livelihoods, particularly for poverty populations, in rural United States communities. Special attention is paid to signifiers of community empowerment and reflexivity as well as other elements of success suggested in the literature. 相似文献
8.
AMY E. POTTER 《Geographical review》2009,99(2):208-230
ABSTRACT. Newspaper articles in the United States paint a picture of Haiti as a failed state, the poorest country in the Western Hemisphere. These articles place the blame of the country's problems entirely on Haiti itself, with little regard for the outside forces that also contributed to the country's present‐day state. This study is a critical geopolitical analysis of Haitian representation in U.S. newspapers. I empirically examine a year's worth of articles from 2004 written in five major U.S. newspapers. From these articles I analyze both the words used to describe Haiti and the emerging media frames. Critical studies have shown that representation in the media can greatly impact the conventional wisdom surrounding a place and legitimize social inequalities. By understanding the images used to describe Haiti, I hope to develop a means of rethinking popular perceptions of the country. I argue that only then can the problems of Haiti be more effectively addressed and a new dialogue created, one that encompasses the entire story of this Caribbean country. 相似文献
9.
PETER J. TALLING LAWRENCE A. AMY RUSSELL B. WYNN CHRISTOPHER J. STEVENSON MICHAEL FRENZ 《Sedimentology》2012,59(6):1850-1887
Current understanding of submarine sediment density flows is based heavily on their deposits, because such flows are notoriously difficult to monitor directly. However, it is rarely possible to trace the facies architecture of individual deposits over significant distances. Instead, bed‐scale facies models that infer the architecture of ‘typical’ deposits encapsulate current understanding of depositional processes and flow evolution. In this study, the distribution of facies in 12 individual beds has been documented along downstream transects over distances in excess of 100 km. These deposits were emplaced in relatively flat basin‐plain settings in the Miocene Marnoso Arenacea Formation, north‐east Italy and the late Quaternary Agadir Basin, offshore Morocco. Statistical analysis shows that the most common series of vertical facies transitions broadly resembles established facies models. However, mapping of individual beds shows that they commonly deviate from generalized models in several important ways that include: (i) the abundance of parallel laminated sand, suggesting deposition of this facies from both high‐density and low‐density turbidity current; (ii) three distinctly different types of grain‐size break, suggesting waxing flow, erosional hiatuses and bypass of silty sediment; (iii) the presence of mud‐rich debrites demonstrating hybrid flow deposition; and (iv) dune‐scale cross‐lamination in fine‐medium grained sandstones. Submarine sediment density flows in basin‐plain settings flow over relatively simple topography. Yet, their deposits record complex flow events, involving transformation between different flow types, rather than the simple waning surges often associated with the distal parts of turbidite systems. 相似文献
10.
AMY MILLS 《Geographical review》2005,95(3):441-462
ABSTRACT. Since the foundation of the Turkish Republic in 1923, when the Turkish nation was defined as ethnically Turkish and Muslim, the issue of ethnic minorities has been at the root of a deep insecurity concerning cultural identity and what it means to be Turkish. The movement to “recover” ethnic minority in history and in place is most visible in Istanbul, the city identified as the location of European culture in Turkey and Turkey's most culturally pluralistic city. The movement has gained pace since the formal acceptance of Turkey as a candidate for membership in the European Union and the push for reforms in human rights. It is promoted by a very small cultural and economic elite and works together with gentrification to produce elite spaces in the city, as exemplified by two neighborhoods: Kuzguncuk, a historic minority neighborhood on the Asian shore of the Bosporus; and “French Street,” a new commercial development in Beyoǧlu, on the European side of the city west of the Bosporus. These landscapes articulate a European, cosmopolitan, and multicultural place identity for Istanbul and reflect a particular notion of Turkey as modern and European, providing insight into the contemporary debate in Turkey concerning the tensions embedded at the core of Turkish cultural identity. 相似文献