Geology and geochronology of the Betara region in south-southeastern Brazil: Evidence for possible Statherian (1.80-1.75 Ga) and Calymmian (1.50-1.45 Ga) extension events

The results of geological mapping, chemical analysis and radiometric dating of metabasic rocks of Betara Formation, and mapping and dating of those present in the Betara basement nucleus together with mylonitic granodiorite and syenogranite are reported here. U-Pb analysis of bulk zircon fractions from the metabasic rocks of the basement nucleus yielded a Statherian age of 1790 +/- 22 Ma, while the metabasic rocks from the upper part of the Betara Formation yielded a Calymmian age between 1500 and 1450 Ma. This age is a minimum for the deposition of the Betara Formation. The older metabasic rocks are associated with post-tectonic, possibly anorogenic syenogranite, while the younger ones are gabbro or very porphyritic ankaramite whose REE patterns are consistent with crystallization from an N-MORB parent magma. The observations and data point to the probable events associated with extensional processes of the end of Paleoproterozoic and early Mesoproterozoic. Similar registers of Statherian (1.80-1.75 Ga) and Calymmian (1.50-1.45 Ga) extensional events are recorded in other parts of the South American and African continents. The Neoproterozoic witnessed the formation and junction of the tectonic slices which formed the Apiai domain during the assemblage of western Gondwana. (C) 2010 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Nd and Pb isotope signatures on the Southeastern South American upper margin: Implications for sediment transport and source rocks

Neodymium and lead isotope values in sediment samples were used to interpret sediment transport and source rocks on the Southeastern South American upper margin. The sediments of the Argentinian margin exhibit an average epsilon(Nd) value of -1.9, indicating the influence of the Andean rocks as sediment sources. Sediments from the Rio de La Plata estuary show an average epsilon(Nd) value of -9.6 which is similar to that of the Southern Brazilian Upper Margin. Finally, sediments of Southeastern Brazil, which are associated with the transport of the Brazil Current exhibit an average epsilon(Nd) of -13.0. The Pb isotope signatures also confirm the differentiation of source rocks in the sedimentation of the study area. In addition, Pb isotopes helped to establish the extent of the influence of the Rio de La Plata on the sedimentation of the Southern Brazilian margin. In terms of Pb isotopes the sediments from the Rio de La Plata estuary and Southern Brazil are more radiogenic than those of Southeastem Brazil and the Argentinian margin. (c) 2007 Elsevier B.V. All rights reserved.

An Analysis of the Telecommunications Business in China by Linear Regression

In this paper, we study the influence of the National Telecom Business Volume by the data in 2008 that have been published in China Statistical Yearbook of Statistics. We illustrate the procedure of modeling “National Telecom Business Volume” on the following eight variables, GDP, Consumption Levels, Retail Sales of Social Consumer Goods Total Renovation Investment, the Local Telephone Exchange Capacity, Mobile Telephone Exchange Capacity, Mobile Phone End Users, and the Local Telephone End Users. The testing of heteroscedasticity and multicollinearity for model evaluation is included. We also consider AIC and BIC criterion to select independent variables, and conclude the result of the factors which are the optimal regression model for the amount of telecommunications business and the relation between independent variables and dependent variable. Based on the final results, we propose several recommendations about how to improve telecommunication services and promote the economic development.

Arctic Tourism: Realities & Possibilities

This paper addresses human capital in the Arctic in relation to tourism. More specifically, with an ever-increasing number oftourists recognizing the attractiveness of the Arctic, tour companies are increasingly recognizing the opportunities. The media(typically southern media) sells the image, either before or after the tourists arrive, and communities are often left to deal with therepercussions – whether those are social, economic, environmental, or the like. Many of the repercussions are negative; however,even when perceived as positive they can create tensions within small communities and showcase a variety of capacity issues.This paper focuses on the realities and possibilities of tourism in the Arctic. It offers an up-to-date descriptive overview of tourismnumbers and valuations. In addition, ‘realities’ also focuses on the current suite of challenges and ‘possibilities’ addresses criticalquestions that need to be asked as tourism grows. We are in an uncertain age and academic critique of the Arctic tourismphenomenon is growing as quickly as the numbers. This paper is almost fully circumpolar in outlook, written by individuals fromthose jurisdictions, and aims to intersect with other sectors active in the Arctic.

Folkmusikundervisningen på fiol och gitarr och dess historiska rötter

How folk musicians of today learn to play their instruments is an over-all question in this article. One violin lesson and one guitar lesson have been observed at Framnäs folk high school. Three research questions were formulated. What do the two lessons have in common? What are the differences? How could the folk music education of today be related to the Swedish fiddler movement in the 1920s and other folk music traditions? Theoretically, the interpretation of the results was based on the mimesis theory of Ricoeur. Two teachers and three students participated in the study. The results showed that the lessons were structured in a similar way and dominated by master apprenticeship teaching. The violin teacher showed a more respectful attitude towards the tradition compared to the guitar teacher. Great parts of the manifest ideology of the fiddler movement seems to have become concealed into a latent or frozen ideology in the formal folk music education of today. There seems to be no big differences between learning the music by way of visiting an older fiddler hundred years ago compared to the study of music today at a formal institution.

Manifesta och latenta ideologier om lärande inom svensk spelmansrörelse under 1920-talet

The purpose of this article was to illuminate existing educational ideologies in the Swedish fiddler movement (Spelmansrörelsen) 1923-1927. This period was characterized by the organization and to some extent institutionalization of Swedish folk music. Furthermore, the purpose was to discuss the results in relation to the folk music education of today. The empirical data was taken from the journal Hembygden, which was a magazine for scholars, enthusiasts and practitioners of folk music. Theoretically, the study was based on a concept of ideology developed by Sven-Eric Liedman: in every time there are two basic forms of identifiable ideology, manifest and latent. From the empirical material as a whole (around 900 articles), a selection was made to find articles dealing with aspects of learning among the fiddlers (33 articles). After content analysis the following themes were generated: Fiddlers’ repertoire, Fiddlers’ masters, Rooms for learning, Learning formation. The writers in Hembygden often emphasized the autodidactic aspects of learning and especially the importance of learning by ear. This manifest ideology of authenticity presumed that learning directly from another fiddler by playing together was to prefer to formal schooling. In spite of a tendency towards more ensemble playing, the folk music education of today in Sweden is characterized by a similar retrospective ideology as in the 1920s.

Tatler (Volume 8 1910)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Lang Syne (Volume 4 1904)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 15 1917)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler a la Guerre (Volume 16 1918)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 14 1916)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 3 1901)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 1 1898)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 13 1915)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.

Tatler (Volume 9 1911)

The Winthrop yearbook was published from 1898 to 2002. It has been known as the Tatler since its inception except for 1904 (Lang Syne) and 1918 (Tatler a la Guerre). No yearbook was published in 1900, 1902, 1903, 1905,1906.