The farnacht formation along the south side of the clew bay fault zone, Western Ireland: Its chemistry and age of metamorphism

2007 ◽  
Vol 23 (3) ◽  
pp. 249-260 ◽  
Author(s):  
M. D. Max ◽  
D. Rex ◽  
J. A. Winchester
Keyword(s):  
Fault Zone ◽  
The South ◽  
South Side ◽  
Western Ireland

scholarly journals Migrated hydrocarbons in basalt on the south side of Scoresby Sund

1984 ◽  
Vol 120 ◽  
pp. 84-85
Author(s):  
W.S Watt ◽  
P Wrang
Keyword(s):  
Fault Zone ◽  
The South ◽  
South Side

A tar-like matenal was found in a fault zone affecting basalt on Savoia Halvø. The material is totally biodegraded but analyses indicate that it is from a raw oil.

On ulug oglum agrïp yok bolča in the Bilgä Kagan Inscription

2020 ◽  
Vol 73 (4) ◽  
pp. 539-550
Author(s):  
Li Yong-Sŏng ◽  
Park Won Kil
Keyword(s):  
The South ◽  
South Side

AbstractThis paper attempts to give new explanation for the expression agrïp yok bol- occurring in 9th line of the south side of the Bilgä Kagan Inscription. After a thorough survey of former research and several Chinese sources, the authors came to the conclusion that this expression must be a euphemistic expression for being beheaded in a battle. The authors found also that kog säŋün was Guo Yingjie 郭英傑. In sum, the sentence in question is to be read as ulug oglum agrïp yok bolča kog säŋünüg balbal tikä bertim ‘When my oldest son died of a disease, I readily erected General Kog as a balbal (for him).’ The expression agrïp yok bol- is to be regarded as a euphemistic expression for being beheaded in a battle.

Heavy minerals solve structural and stratigraphic problems in Ordovician strata of the western Irish Caledonides

2003 ◽  
Vol 140 (1) ◽  
pp. 25-30 ◽  
Author(s):  
MARIA A. MANGE ◽  
JOHN F. DEWEY ◽  
DAVID T. WRIGHT
Keyword(s):  
Island Arc ◽  
Heavy Minerals ◽  
Metamorphic Complex ◽  
The South ◽  
Standard Sequence ◽  
Western Ireland ◽  
Complex Parts ◽  
Wide Horizon

Heavy minerals in Ordovician successions in western Ireland record, in the Upper Arenig Sheeffry Formation, the erosion of an ophiolite/island arc complex. The appearance of staurolite and garnet at a basin-wide horizon in the Lower Llanvirn Upper Derrylea Formation signals the unroofing of the Dalradian metamorphic complex. Parts of the Ordovician sequence on Inishturk and in two small inliers are correlated with the standard sequence with unexpected results. The garnet-, sillimanite-, and staurolite-bearing Letter Formation correlates with the Upper Derrylea Formation and, on Inishturk, heavy minerals in south-younging turbidites reveal a sinistral ramp zone, that places the Sheeffry Formation structurally above and to the south of the younger Derrylea Formation.

scholarly journals Contributions to Marine Bionomics: III. The Systematic Features, Habits, and Respiratory Phenomena of Portumnus nasutus (Latreille)

1897 ◽  
Vol 4 (4) ◽  
pp. 402-407 ◽  
Author(s):  
Walter Garstang
Keyword(s):  
The Other ◽  
The South ◽  
South Side ◽  
Water Spring

The crab whose habits I now describe has not previously been recorded as an inhabitant of British seas. I found two specimens, both male, imbedded in a patch of coarse shell sand on the south side of Drake's Island at low water, spring tides: one on August 11th, 1896, and the other on the following day.

scholarly journals Excavations in Macedonia

1926 ◽  
Vol 6 (1) ◽  
pp. 59-72 ◽  
Author(s):  
Stanley Casson
Keyword(s):  
The South ◽  
Small Stream ◽  
South Side ◽  
South West ◽  
Open Ground ◽  
The Village

The mound of Kilindir (fig. 1) lies about one kilometre south-west of the station of that name on the railway that runs from Salonika to Constantinople via Seres, Dedeagatch and Adrianople. A small stream called Gyol Ayak issues from the south side of Lake Doiran exactly at the modern village at Doiran station. This stream, after passing through nine kilometres of broken and ravined country, issues into more open ground just by the modern Chiflik which represents the pre-war site of the village of Kilindir.

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