Granitoids and greenstones of the White Mfolozi Inlier, south-east Kaapvaal Craton

2020 ◽  
Vol 123 (3) ◽  
pp. 263-276
Author(s):  
A. Hofmann ◽  
H. Xie ◽  
L. Saha ◽  
C. Reinke

Abstract A Palaeoarchaean greenstone fragment and associated granitoid gneisses from an area south of Ulundi in KwaZulu-Natal is described. The fragment consists of an association of garnetiferous amphibolite and calc-silicate that was intruded at 3388 ± 4 Ma by tonalite and at 3275 ± 4 Ma by trondhjemite. Strong ductile deformation of the greenstones and granitoids under amphibolite facies conditions (7 kbar and 600 to 650°C) took place prior to uplift and emplacement of a granite batholith at ~3.25 Ga ago in which the granitoid gneiss-greenstone domain is now found. Magmatism 3.27 to 3.25 Ga ago was a direct response to regional metamorphism and anataxis, and gave rise to stabilization of the southeastern Kaapvaal Craton at that time, earlier than other parts of the craton. Deposition of quartz-arenites on stable granitic basement took place <3.1 Ga ago. Contrasting ages in magmatic pulses and regional metamorphism reflect a different crustal growth history of the eastern and southeastern part of the Kaapvaal Craton.

1998 ◽  
Vol 62 (2) ◽  
pp. 197-212 ◽  
Author(s):  
Anju Tiwary ◽  
Mihir Deb ◽  
Nigel J. Cook

AbstractPyrite is an ubiquitous constituent of the Proterozoic massive sulphide deposit at Deri, in the South Delhi Fold Belt of southern Rajasthan. Preserved pyrite microfabrics in the Zn-Pb-Cu sulphide ores of Deri reveal a polyphase growth history of the iron sulphide and enable the tectono-thermal evolution of the deposit to be reconstructed.Primary sedimentary features in Deri pyrites are preserved as compositional banding. Regional metamorphism from mid-greenschist to low amphibolite facies is recorded by various microtextures of pyrite. Trails of fine grained pyrite inclusions within hornblende porphyroblasts define S1-schistosity. Pyrite boudins aligned parallel to S1 mark the brittle–ductile transformation of pyrite during the earliest deformation in the region. Isoclinal to tight folds (F1 and F2) in pyrite layers relate to a ductile deformation stage during progressive regional metamorphism. Peak metamorphic conditions around 550°C, an estimation supported by garnet–biotite thermometry, resulted in annealing of pyrite grains, while porphyroblastic growth of pyrite (up to 900 µm) took place along the retrogressive path. Brittle deformation of pyrite and growth of irregular pyritic mass around such fractured porphyroblasts characterize the waning phase of regional metamorphism. A subsequent phase of stress-free, thermal metamorphism is recorded in the decussate and rosette textures of arsenopyrite prisms replacing irregular pyritic mass. Annealing of such patchy pyrite provides information regarding the temperature conditions during this episode of thermal metamorphism which is consistent with the hornblendehornfels facies metamorphism interpreted from magnetite–ilmenite geothermometry (550°C) and sphalerite geobarometry (3.5 kbar). A mild cataclastic deformation during the penultimate phase produced microfaults in twinned arsenopyrite prisms.


2013 ◽  
Vol 43 (1) ◽  
pp. 119-130
Author(s):  
Declan William Kavanagh

This essay argues that the work of a lesser-known mid-eighteenth-century satirist Charles Churchill (1731–1764) provides a rich literary source for queer historical considerations of the conflation of xenophobia with effeminophobia in colonial imaginings of Ireland. This article analyzes Churchill's verse-satire The Rosciad (1761) through a queer lens in order to reengage the complex history of queer figurations of Ireland and the Irish within the British popular imagination. In the eighth edition of The Rosciad – a popular and controversial survey of London's contemporary players – Churchill portrays the Irish actor Thady Fitzpatrick as an effeminate fribble, before championing the manly acting abilities of the English actor David Garrick. The phobic attack on Fitzpatrick in The Rosciad is a direct response to Fitzpatrick's involvement in the ‘Fitzgiggo’ riots of January 1763 at the Drury Lane and Covent-Garden theatres. While Churchill's lampooning of the actor recalls Garrick's earlier satirizing of Fitzpatrick as a fribble in The Fribbleriad (1741) and Miss in her Teens (1747), The Rosciad is unique in its explicit conflation of androgyny with ethnicity through Irish classification. The portraiture of Fitzpatrick functions, alongside interrelated axes of ethnicity, class and gender, to prohibit access to a ‘normative’ middle-class English identity, figured through the ‘manly’ theatrical sensibility of the poem's hero, Garrick. Moreover, in celebrating a ‘Truly British Age’, the poem privileges English female players, in essentialist and curiously de-eroticized terms, as ‘natural’ though flawed performers. By analyzing Churchill's phobic juxtaposition of Garrick and the female players against the Irish fribble, this article evinces how mid-century discourses of effeminacy were also instrumental in enforcing racial taxonomies.


BMJ ◽  
1896 ◽  
Vol 1 (1833) ◽  
pp. 397-397
Author(s):  
J. B. Ridley

2011 ◽  
Vol 15 (3) ◽  
pp. 271-278 ◽  
Author(s):  
Graham Livesey

A significant development in urban history was the emergence of the Garden City movement at the end of the nineteenth century, inspired by the writings and actions of Ebenezer Howard. The movement would generate a broad range of urban typologies and various visionary models of the city during the twentieth century. The Garden City was a direct response to what were perceived to be the evils of large industrial cities and attempted to reunite country and town, particularly through the residential garden and the act of gardening. Using Gilles Deleuze and Félix Guattari's assemblage theory I examine gardens and gardening, and the agencies inherent to these. By evoking the early history of the first Garden City at Letchworth, we can ask what role can gardens and gardeners play in addressing contemporary urban issues? [1].


1990 ◽  
Vol 27 (6) ◽  
pp. 731-741 ◽  
Author(s):  
Rudolf Bertrand

Carbonate platform sequences of Anticosti Island and the Mingan Archipelago are Early Ordovician to Early Silurian in age. With the exception of the Macasty Formation, the sequences are impoverished in dispersed organic matter, which is chiefly composed of zooclasts. Zooclast reflectances suggest that the Upper Ordovician and Silurian sequences outcropping on Anticosti Island are entirely in the oil window but that the Lower to Middle Ordovician beds of the Mingan Archipelago and their stratigraphic equivalents in the subsurface of most of Anticosti Island belong to the condensate zone. Only the deeper sequences of the southwestern sector of Anticosti Island are in the diagenetic dry-gas zone. The maximum depth of burial of sequences below now-eroded Silurian to Devonian strata increases from 2.3 km on southwestern Anticosti Island to 4.5 km in the Mingan Archipelago. A late upwarp of the Precambrian basement likely allowed deeper erosion of the Paleozoic strata in the vicinity of the Mingan Archipelago than on Anticosti Island. Differential erosion resulted in a southwestern tilting of equal maturation surfaces. The Macasty Formation, the only source rock of the basin (total organic carbon generally > 3.5%, shows a wide range of thermal maturation levels (potential oil window to diagenetic dry gas). It can be inferred from the burial history of Anticosti Island sequences that oil generation began later but continued for a longer period of geologic time in the northeastern part than in the southeastern part of the island. Oil generation was entirely pre-Acadian in the southern and western parts of Anticosti Island, but pre- and post-Acadian in the northern and eastern parts.


PEDIATRICS ◽  
1953 ◽  
Vol 11 (4) ◽  
pp. 341-357
Author(s):  
WILLIAM G. LENNOX

In a child, a convulsive seizure in association with fever may mean 1 of 6 things. 1. The fever may be a consequence of a spontaneous seizure, the results of an excess of muscular energy and heat. 2. The seizure may be the result of excess hydration or of antibiotics given to combat an infection. 3. The fever may be a seizure phenomenon, the result of a paroxysmal seizure discharge in the region of the hypothalamus. 4. The seizure may be due not to the fever but to bacterial toxins. 5. It may be the secondary result of cerebral pathology induced by an invasion of the brain by the infectious organisms. 6. The seizure may be due to no one of these, but be the direct response of the young child's organism to high fever in association with some infection. In addition, the seizure may not be the consequence of fever, but both fever and seizure a consequence of toxic action on brain cells. Curious features as yet not satisfactorily explained are. 1. Fever-induced seizures belong predominantly to the very young. 2. Almost invariably the febrile seizure, if there is such, is the child's initial seizure. 3. Response to fever is almost invariably a convulsion rather than some other manifestations of epilepsy. A study was made of 1,136 persons whose first convulsive seizure occurred in the first decade of life, 298 having had fever-induced seizures (usually with subsequent non-febrile), 838 having had none. The two groups were compared with respect to age at the first seizure, the presence of antecedent brain pathology, the sex of patients and whether seen in clinic or office. Extreme youth and absence of pathology were most often associated with febrile seizures. Among a total of 407 fever-activated cases, 76.9% subsequently experienced nonfebrile seizures. In 22% an interval of five years or longer separated the last febrile seizure from the first nonfebrile one. With respect to the type of subsequent seizures, an undue proportion of patients had only psychomotor seizures, suggesting that febrile seizures may sometimes be attended by temporal lobe lesions. Febrile seizures are usually innocuous, but if prolonged, focal or attended by much cyanosis or protracted coma, they may cause brain damage. Of 392 patients who sustained brain injury in the first 10 years of life, febrile seizures were blamed for the injury and the continuing epilepsy in 5.4%. Most notable of these findings, however, is the confirmation of what others have reported, that the genetic influence in children having fever-induced seizures is unduly high. In the author's group, this influence, as measured by the incidence of epilepsy among near relatives, is approximately double the genetic influence in young children having only nonfebrile seizures. If we accept the view that evidence of hereditary transmission is the hall-mark of essential epilepsy, then a febrile seizure is epilepsy; but more than that, it is an unusually pure culture of epilepsy. This conclusion has a corollary. Fever-activated epilepsy is short lived. The majority of children with a history of fever-induced seizures have had only one or two. Therefore, the more pure or essential the epilepsy, the better the outlook for spontaneous recovery. Seizures uncomplicated by some acquired pathology of the brain tend to be short lived, perhaps even self-limited—limited by the stabilizing influence of age.


2021 ◽  
Author(s):  
František Hrouda ◽  
Jan Franěk ◽  
Martin Chadima ◽  
Josef Ježek ◽  
Štěpánka Mrázová ◽  
...  

<p>Magnetostatic susceptibility of single crystals of graphite is negative (the mineral is diamagnetic) and strongly anisotropic. The in-phase component of dynamic susceptibility (measured in alternating magnetic field) is also negative, but an order-of-magnitude stronger than the magnetostatic susceptibility. The out-of-phase component, which is no doubt due to electrical eddy currents, is positive and strong. Consequently, if the graphite crystals in graphite ore are oriented preferentially by crystal lattice (LPO), one would expect strong anisotropy of magnetic susceptibility (AMS) of graphite ore in both in-phase (ipAMS) and out-of-phase (opAMS) components. The ipAMS is controlled not only by the LPO of graphite, but also by the preferred orientation of paramagnetic and ferromagnetic minerals of the barren rock, while the opAMS indicates only the LPO of graphite. In graphite ores occurring in the Moldanubian Unit of Southern Bohemia, the in-phase susceptibility ranges from negative values in the order of 10<sup>-5</sup> [SI units] to positive values in the order of 10<sup>-4</sup>. This probably indicates simultaneous control by graphite and paramagnetic and/or ferromagnetic minerals. On the other hand, the out-of-phase susceptibility is much higher, in the order of 10<sup>-4</sup>, and no doubt indicates its graphite control. The degree of ipAMS is moderate, that of opAMS is truly high. The ipAMS foliation is roughly parallel to the metamorphic foliation in ores and wall rocks and the ipAMS lineation is parallel to the mesoscopic lineation. The opAMS is inverse to the ipAMS with the opAMS lineation being perpendicular to the metamorphic foliation. All this indicates a conspicuous LPO of graphite in the ore that was probably created during Variscan regional metamorphism and associated ductile deformation. The opAMS has therefore shown an effective tool for the investigation of the LPO of graphite in graphite ore or graphite-bearing rocks provided that the opAMS is strong enough to be determined with sufficient precision and graphite is the only conductive mineral in the samples investigated.</p>


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