scholarly journals Petrography and illite crystallinity of the Lesser Himalayan metasediments, Gorkha Narayangarh section, central Nepal

1970 ◽  
Vol 14 ◽  
pp. 67-76
Author(s):  
Kabi Raj Paudyal ◽  
Tara Prasad Pokharel ◽  
Lalu Prasad Paudel

Geological study was carried out in the Lesser Himalaya from Gorkha-Narayangarh section of central Nepal aiming to assessthe metamorphism of the area. The area consists of the Kunchha Formation, Fagfog Quartzite, Dandagaon Phyllites, NourpulFormation, Dhading Dolomite, Benighat Slate and the Robang Formation of the Nawakot Complex. Systematic study onpetrography and illite crystallinity was performed in the samples representing all types of lithology and formations. Bothpetrography and illite crystallinity show that the rocks south of Anbu Khaireni belong to chlorite zone. Biotite and garnet zonesare observed only in the north of Anbu Khaireni. The metamorphic zones are inverted as in the other parts of the Lesser Himalaya.DOI: http://dx.doi.org/10.3126/bdg.v14i0.5441Bulletin of the Department of Geology Vol.14 2011, pp.67-76 

2019 ◽  
Vol 58 ◽  
pp. 111-118
Author(s):  
Shrawan Shakya ◽  
Kabi Raj Paudyal

The study was carried out in the Lesser Himalaya between Ridi-Shantipur area of the Gulmi District, west-central Nepal. Two geological units: the Nourpul Formation and the Dhading Dolomite were mapped in the area. These units belong to the Nawakot Group as explained by several researchers in central Nepal. The Nourpul Formation can further be divided into three members based on distinct mappable lithology, which are named as the Lower Member, the Middle Member and the Upper Member, respectively. The area is highly folded with several local and regional anticlines and synclines; Ridi Khola Anticline, Ridi-Karikot Syncline, Ruru Anticline, Baletaksar-Gwadi Syncline, Huga-Bamgha Anticline, Rimuwa-Rudrabeni Syncline, Juhan-Eksing Anticline, Juniya-Limgha Syncline, Bharse-Thaple Anticline, and Chiureko Syncline, respectively from the south to the north. All the folds are trending along to the ESE-WNW direction. The origin of these folds can be linked with the thrust propagation in the Himalaya that can be explained with the deformation event D4. The Harewa Khola Thrust is the only one regional scale thrust mapped in the area. The thrust carries the older Nourpul Formation over the Dhading Dolomite with the indications of thrust related features like slickensides and fault-breccias. The thrust seems to propagate to the north. There is a continuous shear zone mapped in the outcrops from the Tal Khola-Aslewa-Eksingh-Gudrung-Juhang- Rupakot region as an indicator of the presence of the Badi Gad Fault in the region.


1933 ◽  
Vol 33 (4) ◽  
pp. 516-541 ◽  
Author(s):  
G. S. Wilson

1. A systematic study has been made of 165 Brucella strains from different parts of the world, and a less intensive study, comprising only the H2S formation, dye sensitivity, and agglutinin-absorption tests, of a special group of 156 strains from the north-east, east, and south-east of France.2. For purposes of differentiation little weight can be attached to the use of morphological appearances, abundance of growth in culture, pigment formation, the appearance of crystals in the medium, the production of alkali in peptone water, or the utilisation of glucose.3. The presence of 5–10 per cent, of carbon dioxide in the atmosphere is essential for the growth of most freshly isolated bovine abortus strains. This concentration frequently favours the growth of melitensis, though not of porcine abortus, strains. A concentration of 40 per cent. CO2 almost invariably inhibits to some extent the growth of melitensis and porcine abortus strains, and frequently inhibits the growth of bovine abortus strains. It may be concluded that, while the inhibition of growth of a given strain by 40 per cent. CO2 cannot be considered of differential value, the fact that growth in 40 per cent. CO2 is as good as, or better than, that in air is definitely in favour of its being of bovine abortus type, while the occurrence of growth in 10–40 per cent. CO2 but not in air almost certainly indicates that the strain belongs to this type.4. Most bovine abortus, para-abortus, and American porcine abortus strains produce H2S freely for 3 or 4 days, while melitensis, paramelitensis, and Danish porcine abortus strains fail to produce any, or more than a small quantity on the first day only. Though the failure of a given strain to produce H2S cannot be regarded as indicating that it is of melitensis, paramelitensis, or Danish porcine abortus type, the definite production of H2S can be considered as very strong evidence that it is of bovine abortus or American porcine abortus type.5. The dye sensitivity method, introduced by Huddleson, is of very real value in differentiation, and is the only certain method available for distinguishing between the bovine and porcine abortus types. By its means it is possible to divide Brucella strains into three main groups—bovine abortus and para-abortus, porcine abortus, and melitensis and paramelitensis. Not all strains, however, within a given group behave alike, and a number of sub-groups can be established on the basis of special sensitivity to one or more dyes. The method not infrequently yields results that demand considerable experience in their interpretation, and it cannot always be relied upon for the correct typing of individual strains.6. The thermo-agglutination test is one of the simplest methods of detecting antigenic roughness. Any strain that fails to react negatively to this test is unsuitable for the production of smooth antiserum or for use in routine diagnostic agglutination work.7. The agglutinin-absorption method, performed by a strictly quantitative technique, enables a differentiation to be made between bovine and porcine abortus strains on the one hand, and melitensis strains on the other, provided that smooth strains are employed both for the preparation of antisera and for absorption. The use of direct agglutination by monospecific abortus and melitensis sera affords a rapid and accurate means of typing individual strains, and may prove of value in the examination of strains which, while partly rough and unsuitable for absorption experiments, still retain sufficient smooth antigen to be agglutinated by one or other serum. It is also of great service in the detection of mixed strains. Both methods yield identical results.8. In the examination of the main group of strains the serological method proved more valuable than any other method in the correct allocation of individual strains, and the results agreed closely with those afforded by the dye method. In the examination, however, of the special group of strains from the north-east, east, and south-east of France, there was frequently a marked disagreement between the results of the H2S and dye tests on the one hand, and the serological method on the other, the chief divergence being that a number of strains reacting by the former methods as melitensis behaved serologically like abortus. It appears as if, in this particular area of France, strains occur having the metabolic properties of melitensis and the antigenic constitution of abortus.9. A study of the main group of strains by the various methods enumerated enabled them to be classified into the following groups: (a) bovine abortus with five sub-groups, (b) porcine abortus with two sub-groups, (c) melitensis with two sub-groups, (d) para-abortus with two sub-groups, and (e) paramelitensis.10. A study of the special group of strains from the eastern districts of France revealed the presence of ten sub-groups. Since it is rather doubtful to what main group many of the strains belong, they have been classified according to the host from which they were isolated.


2001 ◽  
Vol 25 ◽  
Author(s):  
Santa Man Rai

A multidisciplinary study was carried out in the Lesser Himalaya (LH), the Kathmandu Crystalline Nappe (KCN) and the Gosainkund Crystalline Nappe (GCN) in central Nepal Himalaya. Two principal deformations are recorded in both the crystalline nappes and the Lesser Himalaya: ductile, syn-MCTor syn-MT metamorphic deformation marked by microstructures (stretching lineation, S-C structures, and isoclinal folding) and post-MCT/or post-MT metamorphic deformation recorded by a major EW-directed Likhu Khola anticline and by NNE-SSW-directed folds. The Upper Lesser Himalayan rocks close to the Main Central Thrust (MCT) record syn-MCT metamorphic conditions at 750 MPa and 566 °C. The rocks of the KCN record P-T condition from 900 to 720 MPa and 700 to 484 °C, while the GCN rocks were equilibrated at upper amphibolite- to granulite-facies conditions from 890 to 583 MPa and 754 to 588 °C. The P-T conditions and field observations exhibit well-preserved inverted metamorphism between the Upper Lesser Himalaya and the Gosainkund Crystalline Nappe. The augen gneisses from the GCN yielding 486±9Ma U-Pb zircon age and the granites of similar age in the KCN bear similar petrographic and geochemical characteristics and suggest a similar magmatic origin although they belong to different tectonic units. The chemical analyses of the Proterozoic Ulleri augen gneiss of the LH and the granites of the KCN fall within the same compositional field, indicating a magmatic origin of these augen gneisses. 40Ar/39Ar datings on muscovite indicate cooling ages younging systematically from south to north: 22 to 14 Ma in the KCN, 16 to 5 Ma in the GCN, and 12 to 6 Ma in the LH. This systematic younging of muscovite ages does not have any correlation with the present elevation, lithology and tectonic unit and is interpreted as a result of the exhumation of the rock units on the Main Himalayan Thrust (MHT) ramp situated to the north of Kathmandu Valley. Both the KCN and the GCN record a late emplacement history, but the KCN was exhumed earlier than the GCN. The two crystalline nappes presently form a single tectonic block, and the combined uplift of the two nappes occurs on a ramp of a major decollement developed in the upper part of the Indian crust.


2012 ◽  
Vol 12 ◽  
pp. 242-251 ◽  
Author(s):  
Lalu P Paudel

The Lesser Himalaya in central Nepal comprises low- to medium-grade metasedimentary rocks. Metamorphic studies show that they have experienced at least two metamorphic events (M1 and M2). However, exact timing of metamorphism is still controversial. In the present study K-Ar dating of white micas in shales, slates, phyllites, schists and gneisses from the Tansen-Pokhara section was carried out to understand the timing of metamorphism. The muscovite in gneiss from the MCT zone shows an age of about 1255 Ma representing the age of crystallization of parent granite. Detrital mica from the Bhainskati Formation gives an age of about 2441 Ma. Probably this is the age of crystallization of muscovite in its provenance. The recrystallized white micas from slate and phyllite show older ages (Early Paleozoic) in the southern part (279 to 458 Ma). Most probably this represents the timing of M1. Age become gradually younger towards the north due to the mixing of older (M1 related) and younger (M2 related) white micas. Youngest age (10 Ma) was measured from the sample just below the Upper MCT. This age may be related to the M2 which was due to the Late Miocene-Pleistocene reactivation of the Upper MCT.DOI: http://dx.doi.org/10.3126/njst.v12i0.6509 Nepal Journal of Science and Technology 12 (2011) 242-251


2018 ◽  
Vol 52 (2) ◽  
pp. 455-462 ◽  
Author(s):  
G. Ya. Doroshina ◽  
I. A. Nikolajev

Sphagnum mires on the Greater Caucasus are rare, characterized by the presence of relict plant communities of glacial age and are in a stage of degradation. The study of Sphagnum of Chefandzar and Masota mires is carried out for the first time. Seven species of Sphagnum are recorded. Their distribution and frequency within the North Caucasus are analyzed. Sphagnum contortum, S. platyphyllum, S. russowii, S. squarrosum are recorded for the first time for the study area and for the flora of North Ossetia. The other mosses found in the study area are listed.


2018 ◽  
Vol 69 (2) ◽  
pp. 305-309 ◽  
Author(s):  
Daniela Gitea ◽  
Simona Vicas ◽  
Manuel Alexandru Gitea ◽  
Sebastian Nemeth ◽  
Delia Mirela Tit ◽  
...  

Our study compares the content in polyphenolic compounds and hypericin, in four species of Hypericum - H. perforatum L., H. maculatum Cr., H. hirsutum L., H. tetrapterum Fr. (syn. Hypericumacutum Mnch.) harvested from spontaneous flora in the north-western area of Transylvania, Romania. These species represent an important source of such compounds with different biological actions. After making the extracts, they were subjected to HPLC-SM analysis. The presence of rutoside in the largest amount (462.82 mg %) in the H. perforatum extract was observed, this containing most of the flavonoid heterosides. For the species H. maculatum, the presence in a much higher amount of the hyperoside (976.36 mg %) is characteristic compared to the other species. Quercetol is the best represented of the flavonoid aglycons, its concentration being the highest in H. hirsutum (659.66 mg %). The hypericin content ranges from 0.2171 g % in the H. tetrapterum extract, to 0.0314 g % in the methanol extract of H. maculatum.The highest antioxidant properties measured by FRAP method were recorded in the case of H. perforatum and H. maculatum.


Lithos ◽  
2021 ◽  
Vol 388-389 ◽  
pp. 106060
Author(s):  
Bhupati Neupane ◽  
Junmeng Zhao ◽  
Babu Ram Gyawali ◽  
Yan Deng ◽  
Bishal Maharjan ◽  
...  

Atmosphere ◽  
2021 ◽  
Vol 12 (3) ◽  
pp. 307
Author(s):  
Makoto Inoue ◽  
Atsushi Ugajin ◽  
Osamu Kiguchi ◽  
Yousuke Yamashita ◽  
Masashi Komine ◽  
...  

In this study, we investigated the effects of the Tibetan High near the tropopause and the North Pacific High in the troposphere on occurrences of hot or cool summers in Japan. We first classified Japan into six regions and identified hot and cool summer years in these regions from a 38-year sample (1980–2017) based on the monthly air temperature. To investigate the features of circulation fields over Asia during hot and cool summers in Japan, we calculated the composite differences (hot summer years minus cool summer years) of several variables such as geopotential height, which indicated significant high-pressure anomalies in the troposphere and lower stratosphere. These results suggest that both the North Pacific and the Tibetan Highs tend to extend to Japan during hot summer years, while cool summers seem to be associated with the weakening of these highs. We found that extension of the Tibetan High to the Japanese mainland can lead to hot summers in Northern, Eastern, and Western Japan. On the other hand, hot summers in the Southwestern Islands may be due to extension of the Tibetan High to the south. Similarly, the latitudinal direction of extension of the North Pacific High is profoundly connected with the summer climate in respective regions.


1874 ◽  
Vol 1 (1) ◽  
pp. 1-2
Author(s):  
Edward Hull

This granite forms an isolated mass, rising into two eminences a few miles south of Louisburg, called Corvock Brack (1287 feet) and Knockaskeheen (1288 feet). It is a greyish granite—generally fine—grained—consisting of quartz, two felspars,—one orthoclase, the other triclinic, probably oligoclase—and dark green mica. In some places there are patches in which the felspar assumes the appearance of “graphic granite.” Numerous boulders of this granite are strewn over the district to the north-west, and on the south side of Knockaskeheen; the rock is traversed by regular joints ranging N. 10 W., along which it splits off into nearly vertical walls. The position of the granite is shown on Griffith's Geological Map of Ireland, and it is surrounded by schistose beds, generally metamorphosed, and probably of Lower Silurian age. The granite itself is of older date than the Upper Llandovery beds, which lie to the southward.


2013 ◽  
Vol 20 (1) ◽  
pp. 99-122 ◽  
Author(s):  
Jonathan Fennell

High rates of desertion and surrender during the battles in North Africa in the summer of 1942 were a major factor in Eighth Army’s poor combat performance. At the time, some suggested that these problems were symptomatic of a lack of courage or even of cowardice. There are two broad strands to the conceptualization of courage and cowardice. One focuses on the willingness of the person to fight; the other puts emphasis on how actions express an individual’s ability to cope with fear. Whichever conceptualization is used, high morale motivates the soldier to fight and shields the ordinary recruit from his fear, preventing it from overcoming him in battle. Where morale fails, the soldier is left demotivated and burdened with his terror and, therefore, and is therefore prone to desertion or surrender. Because it is extremely difficult to maintain morale at a continuously high level in an environment governed by chance and managed by humans, all soldiers can find themselves in situations where their actions may be judged as cowardly. Alternatively, if they are properly motivated to fight and prepared by the state and military to deal with the unavoidable fear of combat, all soldiers can be labelled courageous. Accordingly, emotive terms should be avoided when attempting to describe rationally explainable outcomes. The undoubtedly negative connotations attached to cowardice in battle and the positive ones attached to courage are, therefore, arguably unhelpful in understanding Eighth Army’s performance in the summer of 1942 and the human dimension in warfare more generally.


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