scholarly journals Distribution and characteristic features of volcanic rocks in and around the Minami Nagaoka Gas Field from the view point of reservoir geology

2006 ◽  
Vol 71 (1) ◽  
pp. 76-84 ◽  
Author(s):  
Yoshihiro Watanabe
Keyword(s):  
Volcanic Rocks ◽  
View Point ◽  
Gas Field ◽  
Characteristic Features

scholarly journals Fracture Fillings and Implication of Fluid Activities in Volcanic Rocks: Dixi Area in Kelameili Gas Field, Junggar Basin, Northwestern China

Minerals ◽  
2019 ◽  
Vol 9 (3) ◽  
pp. 154 ◽  
Author(s):  
Mingyou Feng ◽  
Tian Liu ◽  
Tong Lin ◽  
Xiaohong Liu ◽  
Ningxin Li ◽  
...  
Keyword(s):  
Carbon Dioxide ◽  
Volcanic Rocks ◽  
Junggar Basin ◽  
Hydrothermal Fluids ◽  
Northwestern China ◽  
Volatile Components ◽  
Gas Field ◽  
Weakly Alkaline ◽  
Quartz Veins ◽  
Calcite Veins

The Carboniferous Batamayineishan Formation of the Kelameili Gas Field is a specific weathered crust-related volcanic reservoir that has a significant production rate in the Junggar Basin, Northwestern China, attributed to debatable processes of fluid evolution. The results suggest that various types of fluids occurring in volcanic rocks lead to the filling of quartz and calcite in fractures and their associated alteration haloes. The silica that formed quartz veins was mainly derived from deep hydrothermal fluids, while the carbon dioxide that formed calcite veins originated from sources characterized by mixing and alteration of deep hydrothermal and hydrocarbon fluids. Siliceous hydrothermal fluids rich in sulphur dioxide and other volatile components were driven by a pressure gradient and buoyancy, and circulated both laterally and vertically along the fractures, forming quartz veins and tension fractures under different temperature conditions. Moreover, changes in salinity, pressure, and carbon dioxide of deep fluids, varying from acidic to weakly alkaline, resulted in earlier calcite precipitation in contraction fractures and weathered fractures. Tectonic uplift resulted in the long-term exposure of volcanic rocks, where fresh water mixed with the partially alkaline fluid escaping the basin to form calcite cements, thus retaining the characteristics of a seepage environment in the weathered fractures. Structural fractures occurred due to tectonic movements during the burial period. Filling and leakage of hydrocarbons caused pore fluids to convert from acidic to alkaline, precipitating late sparry calcite in dissolution fractures. Late hydrothermal fluid metasomatism, brought about by infiltration into the permeable zone, caused partial dissolution of local calcite along cleavage cracks.

scholarly journals Characteristic Features of Districts with Long-Lived Residents as Seen from the Geographical View Point.

1997 ◽  
Vol 47 (2) ◽  
pp. 83-89
Author(s):  
Masamitsu Takatama ◽  
Takashi Watanabe ◽  
Satoru Iesaki
Keyword(s):  
View Point ◽  
Characteristic Features

scholarly journals Chiba Gas Field from the View Point of Development

1964 ◽  
Vol 29 (1) ◽  
pp. 29-38
Author(s):  
Hisao FUJIYAMA ◽  
Takeo HOSHI ◽  
Tsuneo YANAGISAWA ◽  
Kiyotoshi HATA
Keyword(s):  
View Point ◽  
Gas Field

Ultrastructural modification of cellular interactions in cancer tumor

1978 ◽  
Vol 36 (2) ◽  
pp. 318-319
Author(s):  
N. P. Dmitrieva
Keyword(s):  
Cancer Cells ◽  
Human Thyroid ◽  
Adjacent Cell ◽  
Main Role ◽  
Cellular Interactions ◽  
Electron Microscopic ◽  
Cancer Tumor ◽  
Normal Human ◽  
Characteristic Features

One of the most characteristic features of cancer cells is their ability to metastasia. It is suggested that the modifications of the structure and properties of cancer cells surfaces play the main role in this process. The present work was aimed at finding out what ultrastructural features apear in tumor in vivo which removal of individual cancer cells from the cell population can provide. For this purpose the cellular interactions in the normal human thyroid and cancer tumor of this gland electron microscopic were studied. The tissues were fixed in osmium tetroxide and were embedded in Araldite-Epon.In normal human thyroid the most common type of intercellular contacts was represented by simple junction formed by the parallelalignment of adjacent cell membranees leaving in between an intermembranes space 15-20 nm filled with electronlucid material (Fig. 1a). Sometimes in the basal part of cells dilatations of the intercellular space 40-50 nm wide were found (Fig. 1a). Here the cell surfaces may form single short microvilli.

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