Principles and Methods of Zoogeography: The Field Approach

1960 ◽  
Vol 92 (8) ◽  
pp. 636-639
Author(s):  
J. Linsley Gressitt
Keyword(s):  
Field Work ◽  
Complete Understanding ◽  
Field Approach ◽  
History Of

Zoogeographic studies can be pursued in the laboratory or library, but far preferably should be largely based on careful, first-hand field work. A familiarlty with species in the field is a prerequisite to a thorough understanding of both their zoogeography and their systematics. Naturally, knowledge of the actual relationships of the species, and of the geology and geographical history of the areas involved, are also prerequisites to a complete understanding of the zoogeography of a group of insects.

Metasedimentary rocks, intrusions and deformation history in the south-east part of the c. 1800 Ma Ketilidian orogen, South Greenland: Project SUPRASYD 1996

1997 ◽  
pp. 60-65
Author(s):  
Adam A. Garde ◽  
Brian Chadwick ◽  
John Grocott ◽  
Cees Swager
Keyword(s):  
Field Work ◽  
Deformation History ◽  
The South ◽  
Present Contribution ◽  
East Part ◽  
Metasedimentary Rocks ◽  
Deformational History ◽  
Base Camp ◽  
History Of ◽  
Geological Map

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Garde, A. A., Chadwick, B., Grocott, J., & Swager, C. (1997). Metasedimentary rocks, intrusions and deformation history in the south-east part of the c. 1800 Ma Ketilidian orogen, South Greenland: Project SUPRASYD 1996. Geology of Greenland Survey Bulletin, 176, 60-65. https://doi.org/10.34194/ggub.v176.5063 _______________ The south-east part of the c. 1800 Ma Ketilidian orogen in South Greenland (Allaart, 1976) is dominated by strongly deformed and variably migmatised metasedimentary rocks known as the ‘Psammite and Pelite Zones’ (Chadwick & Garde, 1996); the sediments were mainly derived from the evolving Julianehåb batholith which dominates the central part of the orogen. The main purpose of the present contribution is to outline the deformational history of the Psammite Zone in the region between Lindenow Fjord and Kangerluluk (Fig. 2), investigated in 1994 and 1996 as part of the SUPRASYD project (Garde & Schønwandt, 1995 and references therein; Chadwick et al., in press). The Lindenow Fjord region has high alpine relief and extensive ice and glacier cover, and the fjords are regularly blocked by sea ice. Early studies of this part of the orogen were by boat reconnaissance (Andrews et al., 1971, 1973); extensive helicopter support in the summers of 1992 and 1994 made access to the inner fjord regions and nunataks possible for the first time.A preliminary geological map covering part of the area between Lindenow Fjord and Kangerluluk was published by Swager et al. (1995). Hamilton et al. (1996) have addressed the timing of sedimentation and deformation in the Psammite Zone by means of precise zircon U-Pb geochronology. However, major problems regarding the correlation of individual deformational events and their relationship with the evolution of the Julianehåb batholith were not resolved until the field work in 1996. The SUPRASYD field party in 1996 (Fig. 1) was based at the telestation of Prins Christian Sund some 50 km south of the working area (Fig. 2). In addition to base camp personnel, helicopter crew and the four authors, the party consisted of five geologists and M.Sc. students studying mafic igneous rocks and their mineralisation in selected areas (Stendal et al., 1997), and a geologist investigating rust zones and areas with known gold anomalies.

The Ismaili Tradition in Iran: 13th Century to the Present

2021 ◽  
Author(s):  
Daniel Beben
Keyword(s):  
20Th Century ◽  
Future Research ◽  
Early 20Th Century ◽  
13Th Century ◽  
Complete Understanding ◽  
Northern Iran ◽  
Minority Community ◽  
History Of ◽  
The 19Th Century ◽  
To Receive

The Ismailis are a minority community of Shiʿi Muslims that first emerged in the 8th century. Iran has hosted one of the largest Ismaili communities since the earliest years of the movement and from 1095 to 1841 it served as the home of the Nizārī Ismaili imams. In 1256 the Ismaili headquarters at the fortress of Alamūt in northern Iran was captured by the Mongols and the Imam Rukn al-Dīn Khūrshāh was arrested and executed, opening a perilous new chapter in the history of the Ismailis in Iran. Generations of observers believed that the Ismailis had perished entirely in the course of the Mongol conquests. Beginning in the 19th century, research on the Ismailis began to slowly reveal the myriad ways in which they survived and even flourished in Iran and elsewhere into the post-Mongol era. However, scholarship on the Iranian Ismailis down to the early 20th century remained almost entirely dependent on non-Ismaili sources that were generally quite hostile toward their subject. The discovery of many previously unknown Ismaili texts beginning in the early 20th century offered prospects for a richer and more complete understanding of the tradition’s historical development. Yet despite this, the Ismaili tradition in the post-Mongol era continues to receive only a fraction of the scholarly attention given to earlier periods, and a number of sources produced by Ismaili communities in this period remain unexplored, offering valuable opportunities for future research.

scholarly journals Morphology and late Cenozoic (<5 Ma) glacial history of the area between David and Mawson Glaciers, Victoria Land, Antarctica

1994 ◽  
Vol 20 ◽  
pp. 55-60
Author(s):  
Anja L.L.M. Verbers ◽  
Volkmar Damm
Keyword(s):  
Ice Sheet ◽  
Field Work ◽  
Topographic Map ◽  
Glacial History ◽  
Ice Surface ◽  
Victoria Land ◽  
Radio Echo Sounding ◽  
History Of ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Glacio-geological field work and radar ice-thickness sounding were carried out in the area between David and Mawson Glaciers. A subglacial topographic map has been compiled from radio-echo-sounding data. The northern part of this map shows that the trench of David Glacier reaches a depth of more than 1000 m below sea level. The area south of David Glacier comprises a landscape of nunatak clusters dissected by glaciated valleys with ice thicknesses as much as 800 m. Subglacial cirques occur at the outer margins of the nunatak clusters. A model for the regional glacial history is proposed. It starts with a major deglaciation in the Pliocene, which results in marine transgression in basins west of the Transantarctic Mountains. During the late Pliocene, the ice advanced towards the northeast, depositing a thin layer of (Sirius Group) till containing reworked mid-Pliocene marine diatoms. Due to accelerated mountain uplift, the ice cut iIlto the pre-Pliocene peneplain, eroding broad valleys. A period of ice-sheet retreat followed to expose a landscape of large nunataks separated by wide valleys. During this period, local cirque glaciation occurred. When the ice sheet advanced again, another phase of uplift forced the glaciers to cut deeper into the valleys. Probably since the Last Glacial Maximum the ice surface has lowered by about 100 m.

Archaeology in New China

Antiquity ◽  
1963 ◽  
Vol 37 (147) ◽  
pp. 176-184 ◽  
Author(s):  
Hsia Nai
Keyword(s):  
Field Work ◽  
Archaeological Research ◽  
Historical Science ◽  
Considerable Success ◽  
Large Numbers ◽  
History Of ◽  
Ancient Monuments ◽  
Economic Construction ◽  
Abundant Data ◽  
Made In

Archaeology as a branch of historical science has made new headway in the thirteen years since the founding of the Chinese People's Republic. The scale of its work has expanded and methods of research have been improved. Large numbers of young archaeological workers have been trained. In the course of the nation's gigantic economic construction, remains of ancient settlements and tombs have been uncovered in many places, yielding numerous important relics which have provided abundant data for archaeological research. Throughout the country, hosts of archaeological workers from research institutes, universities, museums and institutions for the preservation of ancient monuments are carrying out both field work and academic study and have already attained considerable success in their efforts to explore the history of ancient China on the basis of archaeological finds. All this has given further impetus to the advance of Chinese archaeology.Archaeological finds made in New China are so rich that the present article can attempt to discuss only some of the most important problems.

Spanish Folklore in the Southwest: The Pioneer Studies of Aurelio M. Espinosa

1978 ◽  
Vol 35 (2) ◽  
pp. 219-237
Author(s):  
J. Manuel Espinosa
Keyword(s):  
New Mexico ◽  
Cultural History ◽  
Mexico City ◽  
Golden Age ◽  
Field Work ◽  
Spanish America ◽  
First Century ◽  
Old Spanish ◽  
Cultural Life ◽  
History Of

The centuries-old Spanish folk heritage of our Southwest, and its many faceted and enduring influence on the cultural life of the region, has been written about from various rims of observation. This article describes the pioneer studies of Aurelio M. Espinosa on Spanish folklore in the Southwest, with special emphasis on northern New Mexico. Although he made important contributions to the study of Spanish folklore of southern Colorado, Arizona, and California, and to that of Spain, Mexico, and other parts of Spanish America as well, he devoted most of his research and field work to the upper half of New Mexico which is the richest field of Spanish folklore in the Southwest.In viewing the cultural history of New Mexico, Espinosa reminded his readers that its first century as a Spanish colony, the 17th, was the second great century of Spain's Golden Age of arts and letters. With the vigor of Spain's sense of mission in those centuries, her Golden Age radiated to all parts of Spanish America via Mexico City, Lima, and the other principal colonial capitals. At the same time, from the bookshelf and the store of knowledge of the humble missionary, and the folklore of the Spanish settlers, passed down from generation to generation, the spirit of the Golden Age was reflected on the most remote settled frontiers.

XXVIII.—The Plant Remains in the Scottish Peat Mosses

1906 ◽  
Vol 41 (3) ◽  
pp. 699-723 ◽  
Author(s):  
Francis J. Lewis
Keyword(s):  
Field Work ◽  
Detailed Examination ◽  
Early Autumn ◽  
Peat Deposits ◽  
Plant Remains ◽  
History Of

The following paper deals with an investigation of the successive zones of plant remains contained in the deeper peat deposits covering areas in the Scottish Southern Uplands. The field work was carried on during the summer and early autumn of 1904, and the detailed examination of the peat in the laboratory during part of the winter. No attempt has been made to work out the detailed flora of the different zones, but attention has chiefly been directed to the dominant plant remains found at different horizons in the mosses. Whilst the list of plants from each zone is small, the general facies of the flora of any layer can be gauged from the abundant presence of a few characteristic plants such as Salix reticulata and Empetrum, or Sphagnum and Eriophorum. Thus, while the investigation is incomplete as regards any addition to the history of the British Flora, it will, I hope, throw some light upon the succession of vegetation over the older peat mosses since their origin.

Oil and gas in Kurgan region

2021 ◽  
pp. 9-24
Author(s):  
A. A. Arsenyev ◽  
D. S. Leontiev ◽  
M. D. Zavatsky ◽  
V. V. Saltykov
Keyword(s):  
Oil And Gas ◽  
Field Work ◽  
Research Area ◽  
Petroleum Potential ◽  
Gas Recovery ◽  
History Of ◽  
And Migration ◽  
Active Processes ◽  
Geochemical Studies ◽  
High Degree

This article analyzes the prospects of petroleum potential in Kurgan region. The relevance of the work is due to the high degree of development of the traditional oil and gas recovery areas of Western Siberia, which leads to the need to organize search activities in areas with a low density of hydrocarbon resources. We have analyzed the results of exploratory drilling in the area of the Alabuga river in Kurgan region, and have studied the history of detections of onshore oil occurrences there. Based on the results of the retrospective analysis, the research area was determined, field work was performed to determine the state of search wells in the area, and a collection of geochemical soil and liquid samples was selected. The analysis of the samples revealed that all of them contain methane and its homologues up to and including pentane. The genesis of light methane homologs is related to the processes of catagenesis; their detection on the surface indicates active processes of generation and migration of petroleum hydrocarbons. Based on the analysis of archival materials and estimated ground-based geochemical studies, a conclusion is made about petroleum potential in Kurgan region.

Bonding in Aluminum Phosphate Ceramics Prepared At Low Temperatures

1987 ◽  
Vol 114 ◽  
Author(s):  
Michael R. Silsbee ◽  
D. M. Roy
Keyword(s):  
Phosphoric Acid ◽  
Low Temperatures ◽  
Aluminum Phosphate ◽  
Complete Understanding ◽  
Chemical Binding ◽  
Binding Agents ◽  
History Of ◽  
Alumino Silicate ◽  
Characterization Studies ◽  
History Of Use

ABSTRACTPhosphates have a long history of use as binding agents in ceramic systems. In particular the phosphate bonded alumina refractories and dental cements that employ the chemical reaction between a complex alumino-silicate glass and a buffered phosphoric acid to produce binding are among the most well known.The work described here has been undertaken in an effort to achieve a more complete understanding of the nature of the chemical binding in these materials.The results of a series of characterization studies on materials from the Al2O3-P2O5-H2O and SiO2-Al2O3-P2O5-H2O systems will be discussed with particular emphasis on the nature of the binding produced in these materials.

Aerial Reconnaissance of the Fen Basin

Antiquity ◽  
1945 ◽  
Vol 19 (75) ◽  
pp. 145-153
Author(s):  
F./Lt. D. N. Riley
Keyword(s):  
Field Work ◽  
Early History ◽  
Amount Of Information ◽  
Vast Amount ◽  
Aerial Reconnaissance ◽  
History Of

Aerial reconnaissance and photography are of great importance in the study of the early history of Fenland and the surrounding country, conditions often being A very suitable for this method of investigation. A vast amount of information which can be recorded easily by air-photography, would only be obtained with the greatest difficulty, if at all, by field-work on the ground. The present paper is a brief record of observations made while flying over the fen basin during the course of duty. Unfortunately photography was not practicable, but systematic notes were kept of everything observed. Further work should reveal much more.

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