1 v. : illus., mapsRock magnetism is the study of the magnetic properties of rocks, and palaeomagnetism forms one branch of this discipline. Palaeomagnetism is concerned with the natural ("fossil") remanent magnetization of rocks with the particular objective of studying the Earth's magnetic field during the geological past, The study is based on the supposition that a rock acquires a remanence at the time of its formation, the direction of which is parallel to the Earth's field, so that it is possible to infer the direction of the Earth's field at the time of the formation of the rock by an examination of its remanent magnetization. The intensity of magnetization is related with the strength of the Earth's field at that time, but in a complex manner, and most palaeomagnetic work is concerned with the directions of remanent magnetization. (First paragraph of introduction)
A systematic palaeomagnetic study in the eastern part of the Trans-Mexican Volcanic Belt includes 39 Miocene,
Pliocene and Quaternary volcanic rocks in the southeastern Mexico Basin (Sierra Nevada and Sierra de Rı´o Frı´o),
the Altiplano area, and the Palma Sola Massif. A total of 430 samples have been selectively demagnetized using
mostly alternating field demagnetizing methods, supplemented by thermal analyses. Most characteristic remanences
are carried by low-Ti titanomagnetites, with occasional titanohematites or slightly maghemitized low-Ti titanomagnetites,
of similar direction. Seven sites were discarded because they presented intermediate directions, hydrothermal
alteration or were remagnetized by lightning strikes. The mean directions of 32 sites, together with 24 sites from
Sierra de las Cruces in the western Mexico basin, indicate rocks older than 2 Ma are rotated some 10° counterclockwise
with respect to Quaternary rocks, whereas there is no rotational difference between Miocene and Pliocene rocks.
Statistical analyses between different regrouped populations confirm that the rotational pattern is due to the age of
the volcanics rocks but not to their spatial distribution. The Quaternary mean direction from the three Mexico Basin
ranges is consistent with the geographical reference pole. In contrast, the Pliocene mean direction from volcanic rocks
of the Altiplano area and the Sierra de Las Cruces is slightly rotated some 10° westwards with respect to the reference
direction from North America. No significant rotations have been observed in the eastern TMVB (from the western
Mexico Basin to the border of the Altiplano), between late Miocene and late Pliocene times. It suggests that a very
small, counterclockwise vertical-axis rotation may have been taken place in this segment of the TMVB between late
Pliocene and Quaternary times. Comparisons of these results with a summary of the available palaeomagnetic data
in the area indicate that the previously reported Quaternary rotations are of questionable reliability, and that the
large counterclockwise rotations, reported in Cretaceous to Miocene rocks, probably took place before the late
Miocene. These new palaeomagnetic data support the idea that the eastern TMVB since the late Miocene, has been
a zone of extension with a little, left-lateral shear component
This paper explores competing accounts of an apparent inversion of the previously-prevailing relationship between young people's unemployment and the incidence of youth offending at a time of economic recession. It begins by highlighting the faltering association between unemployment and offending, and considers the paradoxical implications for risk-based methodologies in youth justice practice. The paper then assesses explanations for the changing relationship that suggest that youth justice policies have successfully broken the unemployment-offending link; and alternatively that delayed effects of recession have yet to materialise, by reference to the work of four Inter-governmental organisations and to youth protests beyond the UK. In place of ever more intensive risk analyses, the paper then focusses on the adverse effects of unemployment on social cohesion, and proposes a rights-based approach to youth justice that recognises the growing disjuncture between the rights afforded to young people and the responsibilities expected of them
Meteorites have a hot origin as planetary materials derive from a supernova, similar to SN1987A, and were acquired by a nearby nova, the Sun. The supernova plasmas became zoned around the nova, mainly by their electromagnetic properties. Carbon and carbide dusts condensed first, followed, within the Inner Planetary Zone, by Ca–Mg–Al oxides and then by iron and nickel metal droplets. In the inner Asteroid Belt, the metals aggregated into clumps as they solidified but over a much longer time in the Inner Zone. ‘Soft’ collisions formed larger (<∼20 km) objects in the Asteroid Belt; in the Inner Zone these aggregated forming proto-planetary cores during inwards orbital migration. In the Asteroid Belt, glassy olivines condensed, followed more open lattice minerals growing grew primarily by diffusion. Brittle silicate crystals were comminuted and only aggregated into the carbonaceous meteorites when water–ices formed. The inner planets differentiated by at least 4.4 Ga. Jupiter and the outer planets grew on asteroidal bodies thrown out into freezing water vapours and only formed by 4.1 Ga, resulting in the Late Heavy Bombardment, initially by meteoritic materials and later supplemented by ices from, and beyond, the Asteroid Belt. Critical factors are the properties of very high temperature supernova plasmas, the duration of the molten iron phase in the inner zone. Evidence usually quoted for a cold origin derives from late stage processes in hot meteorite evolution. While highly speculative, it is shown that meteorites and planets can be formed by known processes as supernova plasmas cool
New Palaeomagnetic data for 30 sites (271 samples) and K–Ar data from five units in the Sierra de Las Cruces,
western Basin of Mexico, provide constraints on the spatial-temporal evolution of arc magmatism in the central
Trans-Mexican Volcanic Belt. The normal and reversed directions show a polarity pattern with a consistent spatial
zonation perpendicular to the NNW–SSE trend of the range. The magnetostratigraphy and K–Ar dates indicate that
volcanic activity in the Sierra de Las Cruces migrated southeastward at a mean rate of 1.6 cm/a, between 3.6 and
1.8 Ma, and that the rate of migration may have been higher, up to 4 cm/a, during the Gauss Chron. Normal and
reversed directions pass the reversal test at a 95% confidence level. The mean Plio-Quaternary palaeomagnetic
direction for Sierra de Las Cruces is D=350.7°, I=30.6° (N=25, k=30.7, α95=5.3°). The declination deviates to the
west of the expected direction, which suggests that small counterclockwise rotations could take place during formation
of the Sierra de Las Cruces volcanics
BARRY CUNLIFFE. Europe between the Oceans: Themes and Variations: gooo BCAD 1000. New Haven, C T and London: Yale University Press, 2008. Pp. ix, 518. 39.95(US).ReviewedbyMartinW.LewisAYSEDEVRIMATAUZ.EightThousandYearsofMalteseMaritimeHistory:Trade,Piracy,andNavalWarfareintheCentralMediterranean.Gainesville,FL:UniversityPressofFlorida,2008.Pp.xiv,379.69.95 (US). Reviewed by Victor Mallia-Milanes
IAN WORTHINGTON. Philip II of Macedonia. New Haven, CT and London: Yale University Press, 2008. Pp. xx, 303. 35.00(US).ReviewedbyCraigeB.ChampionFEDERICOSANTANGELO.Sulla,theElites,andtheEmpire:AStudyofRomanPoliciesinItalyandtheGreekEast.Leiden:Brill,2007.Pp.xix,230.€99.00.ReviewedbyArthurM.EcksteinROSAMONDMCKITTERICK.Charlemagne:TheFormationofaEuropeanIdentity.NewYork,NY:CambridgeUniversityPress,2008.Pp.xviii,460.29.99 (US), paper.Reviewed by David S. Bachrach
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