scholarly journals Geology and petrology of the red wine alkaline complex, central Labrador

1981 ◽  
Author(s):  
L W Curtis ◽  
K L Currie
Keyword(s):  
Red Wine ◽  
Alkaline Complex

Correlation of two Helikian peralkaline granite – volcanic centres in central Labrador

1983 ◽  
Vol 20 (5) ◽  
pp. 753-763 ◽  
Author(s):  
J. D. Hill ◽  
A. Thomas
Keyword(s):  
Red Wine ◽  
Lake Superior ◽  
Volcanic Complex ◽  
Continental Rifting ◽  
Alkaline Complex ◽  
Peralkaline Granite ◽  
Space And Time ◽  
Terrestrial Sediments ◽  
Grenvillian Orogeny ◽  
Intrusive Suite

Recent mapping in central Labrador has resulted in the recognition and correlation of two Neohelikian peralkaline silicic igneous centres. The Flowers River igneous suite is circular in shape, covers an area of approximately 1720 km2, and consists of undeformed comenditic granite in contact with extrusive equivalent porphyry, felsite, tuff, and breccia. The Letitia Lake volcanic complex has been deformed by the Grenvillian Orogeny into an elliptical structure that covers approximately 450 km2. The complex consists of comenditic granite and syenite of the Arc Lake intrusive suite and related porphyry, rhyolite, tuff, and volcanogenically derived sediments of the Letitia Lake Group. Undersaturated aenigmatite–nepheline gneisses and syenites of the Red Wine alkaline complex are associated in space and time with the peralkaline silicic rocks of the Letitia Lake complex. The two centres are separated by 175 km and are an integral part of a Neohelikian period of uplift and continental rifting that involved formation of plateau basalts, terrestrial sediments, diabase dikes, and peralkaline magmatic centres in a belt extending from south Greenland to Lake Superior.

Red Wine Color

2004 ◽  
Keyword(s):  
Red Wine ◽  
Wine Color

Endothelin-1 synthesis reduced by red wine

Nature ◽  
2001 ◽  
Keyword(s):  
Red Wine ◽  
Endothelin 1

Element and redox homeostasis in rats after red wine consumption

2011 ◽  
Vol 49 (05) ◽  
Author(s):  
K Szentmihályi ◽  
Z May ◽  
H Fébel ◽  
G Bekő ◽  
A Blázovics
Keyword(s):  
Red Wine ◽  
Redox Homeostasis ◽  
Wine Consumption

Red wine increases SHBG production by HepG2 cells

2014 ◽  
Author(s):  
Cristina Saez Lopez ◽  
Rafael Simo ◽  
Cristina Hernandez ◽  
David Martinez Selva
Keyword(s):  
Hepg2 Cells ◽  
Red Wine

Red wine extract, resveratrol, on maintenance of organ function following trauma-hemorrhage

2012 ◽  
Vol 2 (10) ◽  
pp. 351
Author(s):  
Fu-Chao Liu ◽  
Huang-Ping Yu
Keyword(s):  
Intracellular Signaling ◽  
Red Wine ◽  
Antioxidant Properties ◽  
Neutrophil Function ◽  
Protective Effects ◽  
Organ Function ◽  
Mitogen Activated Protein ◽  
Ros Formation ◽  
Anti Inflammatory ◽  
And Control

Resveratrol, is a polyphenol that can be extracted from grapes and red wine, possess potential anti-inflammatory effects, which would result in the reduction of cytokine production, the alteration of the expression of adhesion molecule molecules, and the inhibition of neutrophil function. Resveratrol might also act as an antioxidant, anti-aging, and control of cell cycle and apoptosis. Resveratrol has been shown to have protective effects for patients in shock-like states. Such protective phenomenon is reported to be implicated in a variety of intracellular signaling pathways including the regulation of the mitogen-activated protein kinases (MAPK)/ hemeoxygenase-1 (HO-1) pathway, activates estrogen receptor (ER), and the mediation of pro-inflammatory cytokines, reactive oxygen species (ROS) formation and reactive. Moreover, through anti-inflammatory effects and antioxidant properties, the resveratrol is believed to maintain organ function following trauma-hemorrhage.Key words: resveratrol, anti-inflammatory, trauma-hemorrhage.

A review of the composition and evolution of hydrocarbon gases during solidification of the Ilímaussaq alkaline complex, South Greenland

2001 ◽  
pp. 159-166 ◽  
Author(s):  
Jens Konnerup-Madsen
Keyword(s):  
Nepheline Syenite ◽  
Subsequent Development ◽  
High Water ◽  
Vapour Phase ◽  
Low Carbon ◽  
Low Oxygen ◽  
Alkaline Complex ◽  
Hydrocarbon Gases ◽  
Wide Range ◽  
Water Contents

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Konnerup-Madsen, J. (2001). A review of the composition and evolution of hydrocarbon gases during solidification of the Ilímaussaq alkaline complex, South Greenland. Geology of Greenland Survey Bulletin, 190, 159-166. https://doi.org/10.34194/ggub.v190.5187 _______________ Fluid inclusions in minerals from agpaitic nepheline syenites and hydrothermal veins in the Ilímaussaq complex and in similar agpaitic complexes on the Kola Peninsula, Russia, are dominated by hydrocarbon gases (predominantly methane) and hydrogen. Such volatile compositions differ considerably from those of most other igneous rocks and their formation and entrapment in minerals reflects low oxygen fugacities and a wide range of crystallisation temperatures extending to a low-temperature solidus. Their composition reflects initial low carbon contents and high water contents of the magma resulting in the exsolution of a waterrich CO2–H2O dominated vapour phase. Fractionation of chlorides into the vapour phase results in high salinities and the subsequent development of a heterogeneous vapour phase with a highly saline aqueous-rich fraction and a methane-dominated fraction, with preferential entrapment of the latter, possibly due to different wetting characteristics. The light stable isotope compositions support an abiogenic origin for the hydrocarbons in agpaitic nepheline syenite complexes.

Natrophosphate from the Ilímaussaq alkaline complex, South Greenland

2001 ◽  
pp. 139-141
Author(s):  
Ole V. Petersen ◽  
Alexander P. Khomyakov ◽  
Henning Sørensen
Keyword(s):  
Refractive Index ◽  
Kola Peninsula ◽  
Unit Cell Parameter ◽  
Cell Parameter ◽  
Water Soluble ◽  
Type Locality ◽  
Drill Core ◽  
Alkaline Complex ◽  
First Time ◽  
Alkaline Complexes

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Petersen, O. V., Khomyakov, A. P., & Henning. (2001). Natrophosphate from the Ilímaussaq alkaline complex, South Greenland. Geology of Greenland Survey Bulletin, 190, 139-141. https://doi.org/10.34194/ggub.v190.5184 _______________ The rare mineral natrophosphate has been identified for the first time in the Ilímaussaq alkaline complex in a drill core from the Kvanefjeld area. It occurs sparsely in zoned veinlets with cores of natrophosphate and borders of fibrous trona. The natrophosphate is more or less smoky, transparent and unaltered. The refractive index n = 1.448 ± 0.005 is low compared to that given for the material from the type locality, Khibina alkaline complex, Kola Peninsula; the unit cell parameter a = 27.76 ± 0.05 Å is in excellent agreement with that given for the material from the type locality. The veins occur in hyper-agpaitic naujakasite lujavrite; villiaumite is an associated mineral. Only a few water-soluble minerals have so far been found in the Ilímaussaq alkaline complex compared to the wealth of such minerals in the Khibina and Lovozero alkaline complexes. This is possibly at least partly due to lack of necessary precautions during sampling.

Identification of Antioxidant Products from Plasma Treated Red Wine

2019 ◽  
Vol 48 (8) ◽  
pp. 909-914
Author(s):  
Gyeong Han Jeong ◽  
Tae Hoon Kim
Keyword(s):  
Red Wine
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