scholarly journals Mineralogy and Geochemistry of Titaniferous Gabbros of Ophiolitic Fanouj Zone (Sistan & Baluchestan, Iran)

2016 ◽  
Vol 10 (4) ◽  
pp. 189 ◽  
Author(s):  
Majid Falaknazi ◽  
Mehrdad Karimi
Keyword(s):  
Crystallization Process ◽  
The West ◽  
Ophiolite Complex ◽  
Tholeiitic Magma ◽  
Incompatible Elements ◽  
South West ◽  
West Part ◽  
Main Host ◽  
Uplift Zone ◽  
Compatible Elements

<p><span lang="EN-US">Ophiolite complex in the west of Fanuj is 200 Km south west of Iranshahr in Sistan and Baluchestan province. This ophiolite complex lies in the uplift zone of the oceanic crust of Oman between Makran and Fanuj faults. Ophiolite of the west part of Fanuj is consisted of three parts including gabbro, diabase dikes and small quantity microdiorite masses. Ilmenite is the main mineral of titanium which along with magnetite has been formed independently or inter-crystalline way after crystallization of plagioclase, pyroxene and often along with amphibole in gabbro rocks. The formation of the broad gabbro masses which is associated with plagioclase and pyroxene crystallization in High Oxygen fugacity condition formed a fluid rich in iron and titanium during the formation of ferro gabbro rocks as the main host of the ilminite reserves. Gradual crystallization process and decrease in compatible elements such as </span><span lang="EN-US">Cr, Ni, Mg and increase in incompatible elements such as Mn</span><span lang="FA" dir="RTL">،</span><span lang="EN-US"> Na</span><span lang="FA" dir="RTL">،</span><span lang="EN-US"> Ti from the bottom to the upper parts of ophilite complex shows that </span><span lang="EN-US">the formation of the complex has been occurred through the process of crystal fractionation from a tholeiitic magma which is rich in titanium.</span></p>

Epizootology (epidemiology) of helminthozoonoses in the south-west of Republic of Kazakstan

2018 ◽  
Vol 12 (2) ◽  
pp. 27-32
Author(s):  
S.A. Kenzhebaev ◽  
D. Ibragimov ◽  
G.O. Zhumalieva
Keyword(s):  
Physiological State ◽  
Postmortem Examination ◽  
Health Statistics ◽  
The South ◽  
The West ◽  
South West ◽  
West Part ◽  
Regional Specificity ◽  
Examination Methods ◽  
Cysticercus Bovis

The purpose of the research: to educe regional specificity of epizootology (epidemiology) of helminthozoonoses (taeniarinhosis - cysticercosis, echinococcosis, trichinellosis) in Kyzylorda region Republic of Kazakstan. Materials and methods. In 2010-2016 according to postmortem examination methods cattle is investigated on cysticercosis and echinococcosis, sheep camels and horses on echinococcosis, pigs on taeniasis saginata at the premises of Kyzylorda meat cutting plant and at Kyzylorda markets. Physiological state of cysticercuses and caseworm larvocyst have been studied depending on the animal age. Invasion extensiveness (IE) of dogs were studied by the method of control worming by hydrobromide arecoline. As well as veterinarian and medical audit in region for the last 10 years was analyzed. Results and discussion. It has been established that cysticercosis bovine is widespread endemic and irregular. Invasion extensiveness (IE) of cattle was higher on the south-east of region (3.3%), and on the west this measure greatly declined (2.4%). This zoonosis extensiveness is greatly progressed during last 7 years (from 1.7% in 2010 till 3.3% in 2016). In general, at the south-west part of Kazakstan cattle is infected by Cysticercus bovis on 2.6-2.9% while the invasion strength (IS) is average 2-4 cysticercuses onto one corpse. During 2010-2016 it was educed two persons who are ill on taeniasis saginata. Sheep, cattle and camels were average taken by caseworms on 21.1%, 8.1%, and 42.7% respectively. IE parameters depended on the age and were high at the adult animals: Lambs are wormy on 2.5%, sheep older then 5 years on 29.5%, young camels at the age under 2 years are wormy on 27.9%, and animals older then 7 years on 50.0%, calves under 2 years are wormy on 2.4%, and cattle older then 5 years on 10.7%. IS of all kinds of animals correlated outright to EI and also depended on the animal age. In the process of internal veterinarian sanitary examination of 1680 killing horses of different age caseworm larvocyst were not founded. According to the data from health statistics, 463 patients (including 47.7% of men and 52.6% of women) have been operated concerning caseworm in the clinics in Kyzylorda region during 12 years (2005-2016 years). In 2010-2016 it was tested 688 samples of muscles of imported pork for trichinellosis by compressor method. All samples were negative. Over the last 10 years caseworm of animal and human was not registered in the region except one outburst in 2016 (February-March), during which 20 accidents of human caseworm had been educed in the region. The source of invasion was wild boars meat.

Excavations in Midea 2007

2009 ◽  
Vol 2 ◽  
pp. 7-30 ◽  
Author(s):  
Katie Demakopoulou ◽  
Nicoletta Divari-Valakou ◽  
Monica Nilsson ◽  
Ann-Louise Schallin
Keyword(s):  
Bronze Age ◽  
Early Phase ◽  
The West ◽  
Large Section ◽  
Ample Evidence ◽  
West Part ◽  
Large Opening

Excavations in Midea continued in 2007 as a Greek-Swedish programme under the direction of Dr Katie Demakopoulou in collaboration with Dr Ann-Louise Schallin. In the West Gate area excavation continued in the west part of the building complex that abuts the fortification wall. Room XIV was excavated with abundant remains of LH IIIB2 pottery. A sealstone with a unique, possibly ritual, scene was also found. On the lower west terrace of the acropolis excavation continued in Trench C, where a large section of the fortification wall was uncovered. Room I was excavated here, adjacent to the inner face of the fortification wall. Finds in this room date to the early phase of LH IIIC, under which there was ample evidence of the LH IIIB2 destruction, including human skeletons. Under this debris, a large opening leading to a gallery or syrinx through the thickness of the fortification wall was found. Excavation was resumed also in the East Gate area, where a new wall was revealed in the baulk between Trench 3 and Room 9. The wall is perpendicular to the citadel wall and borders Trench 3. Excavation was also resumed in Trenches 9 and 14. The latest Mycenaean material in this area dates to LH IIIB2, but there is evidence of post-Bronze Age activity, which is demonstrated mainly by pottery finds.

Peregrinação Acadêmica: A mulher Romeira do Bom Jesus da Lapa

2020 ◽  
Author(s):  
Sandra Célia Coelho Gomes da Silva
Keyword(s):  
Gender Identity ◽  
Social Reproduction ◽  
Participant Observation ◽  
Female Gender ◽  
Age Group ◽  
Structured Interviews ◽  
The West ◽  
Patriarchal Family ◽  
The Family ◽  
West Part

This work is the result of the doctoral thesis entitled Pilgrimage of Bom Jesus da Lapa: Social Reproduction of the Family and Female Gender Identity, specifically the second chapter that talks about women in the Pilgrimage of Bom Jesus da Lapa, emphasizing gender relations, analyzing the location of the pilgrimage as a social reproduction of the patriarchal family and female gender identity. The research scenario is the Bom Jesus da Lapa Pilgrimage, which has been held for 329 years, in that city, located in the West part of Bahia. The research participants are pilgrim women who are in the age group between 50 and 70 years old and have participated, for more than five consecutive years in the Bom Jesus da Lapa Pilgrimage, belonging to five Brazilian states (Bahia, Minas Gerais, São Paulo, Espírito Santo and Goiás) that register a higher frequency of attendance at this religious event. We used bibliographic, qualitative, field and documentary research and data collection as our methodology; we applied participant observation and semi-structured interviews as a technique. We concluded that the Bom Jesus da Lapa Pilgrimage is a location for family social reproduction and the female gender identity, observing a contrast in the resignification of the role and in the profile of the pilgrim women from Bom Jesus da Lapa, alternating between permanence and the transformation of gender identity coming from patriarchy.

Mosses and lichens of Shokalsky Island (Kara Sea, Yamal-Nenets Autonomous Area)

2020 ◽  
Vol 54 (2) ◽  
pp. 497-513 ◽  
Author(s):  
L. N. Beldiman ◽  
I. N. Urbanavichene ◽  
V. E. Fedosov ◽  
E. Yu. Kuzmina
Keyword(s):  
Plant Communities ◽  
Species Distribution ◽  
Arctic Tundra ◽  
Kara Sea ◽  
Lichenicolous Fungi ◽  
South West ◽  
West Part ◽  
First Time ◽  
Nenets Autonomous ◽  
Made In

We studied in detail a moss-lichen component of Shokalsky Island vegetation for the first time and identified 79 species of mosses and 54 species and 2 subspecies of lichens and lichenicolous fungi. All species of mosses and 23 species and 2 subspecies of lichens and lichenicolous fungi are recorded for the first time for the island. The study is based on collections made in South West part of the island, in arctic tundra. We also explored the participation of the mosses and lichens in the main types of plant communities and the species distribution in 10 ecotopes. The paper describes the noteworthy findings (Abrothallus parmeliarum, Aongstroemia longipes, Arthonia peltigerea, Caloplaca caesiorufella, Catillaria stereocaulorum, Ceratodon heterophyllus, Lecanora leptacinella, Sphagnum concinnum, S. olafii) and features of bryo- and lichenoflora of Shokalsky Island.

The Base and Top of the Coral-rock in Barbados

1937 ◽  
Vol 74 (8) ◽  
pp. 337-359 ◽  
Author(s):  
C. T. Trechmann
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
East Part ◽  
Varying Thickness ◽  
South West ◽  
New Information ◽  
Main Portion ◽  
Coral Rock

1. The coral-rock commences nearly everywhere with a basal bed of varying thickness containing a fauna of pre-Pleistocene aspect among which the genus Haliotis (absent from these coasts at the present day), Pleurotomaria, Meiocardia, etc., are noticeable. This faunule may have lived at a depth of 700–1,000 feet.2. The supposition that the southerly anticlines are a later uplift than the main portion of Barbados is supported by the absence of ravines, and the presence of post-coral-rock beds which occur as coastal veneers at low altitudes, and in greater thickness in the south-east corner near Whitehaven.3. The south-east part of the island from Consett Point to Ragged Point has probably extended further seawards in comparatively recent times ; the series of converging faults and dislocations in the cliff sections suggest that the thrusts from the west or south-west may have been resisted by this part of the island.4. The relative claims of fault-scarping or marine erosion in production of the rising terraces is discussed ; and new information regarding the thickness of the coral-rock at sea-level from a boring is detailed.5. The finding of a faunule with Pliocene or possibly Miocene affinities at the base of the coral-rock puts the Oceanic series further back, into the Miocene.

scholarly journals The Results of a Chemical, Microscopical and Bacteriological Examination of Samples of London Milks

1907 ◽  
Vol 7 (1) ◽  
pp. 22-31 ◽  
Author(s):  
R. Tanner Hewlett ◽  
George S. Barton
Keyword(s):  
Bacteriological Examination ◽  
Milk Supply ◽  
The South ◽  
The West ◽  
The North ◽  
South West ◽  
Pure Milk

In view of the importance of a pure milk supply, we considered that it might be of interest to examine chemically, microscopically, and bacteriologically, a number of specimens of milk coming into the Metropolis for which purpose we decided to select samples from the various counties, the milk of which is consigned to London. We found that milk so consigned comes from about twenty-six counties extending from Derby in the North, to Hampshire and Devonshire in the South and South-West, and from Hereford in the West, to Norfolk in the East.

scholarly journals The Mackerel Fishery in the West of England

1889 ◽  
Vol 1 (1) ◽  
pp. 72-73 ◽  
Author(s):  
R. J. Ridge
Keyword(s):  
The West ◽  
South West ◽  
Stormy Weather

The mackerel fishery began off Plymouth in January, and boats from Yarmouth, Lowestoft, Newhaven, Brighton, Eastbourne, Hastings, Plymouth, together with a considerable number of Mount's Bay boats (Porthleven, Newlyn, and Mousehole) were engaged in the above fishery. Fish were found about the 13th January fifteen to twenty-five miles south-west of the Start Point, of a very fine quality, and were caught in considerable quantities for some few nights, catches from two lasts (20,000) down to few hundreds per boat. Westerly and south-west winds prevailing (strong breezes), very stormy weather set in, and fishing operations were interrupted for three weeks, when the boats got to work again, meeting only with light catches for some weeks, February and March were not very successful months, easterly winds set in and continued throughout above months, and practically nothing was done till latter part of March and beginning of April, when boats fell in with fish south-west of Eddystone fifteen to twenty-five miles. There fish were not so fine in quality as those of January, and appeared to be quite distinct from the latter. Some good hauls were secured, one last (being about the largest catch) to few hundreds per boat. The fishing continued up to May, and boats did fairly well, a good average earnings was obtained, prices kept up, especially during Lent.

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