
Leucogranite - Wikipedia
Leucogranite is a light-colored, granitic, igneous rock containing almost no dark minerals. Leucogranites have been reported from a variety of orogenies involving continental collisions.
Alaskite: Mineral information, data and localities. - mindat.org
The term is used to designate granitoid rocks in which quartz constitutes 20% to 60% of the felsic minerals and in which the ratio of alkali feldspar to total feldspar is greater than 90%; i.e., the …
白岗质花岗岩 - 百度百科
白岗质花岗岩(Alaskite)是采集于黑龙江省伊春市嘉荫县孙吴-嘉荫盆地的岩石标本。 灰白色,中粗粒结构,块状构造,主要矿物成分:石英、斜长石、角闪石,暗色矿物含量极少。 [1] 可用 …
ALASKITE Definition & Meaning - Merriam-Webster
The meaning of ALASKITE is a leucocratic granite of medium or fine grain composed chiefly of quartz and alkali feldspars.
白岗岩 - 《中国大百科全书》第三版网络版
2022年1月20日 · 白岗岩是制造玻璃与陶瓷的原料,在陶瓷生产中主要用于坯体制造。 白岗岩标本. 桑隆康,马昌前.岩石学 . 2版.北京:地质出版社,2012..
Alaskite-type uranium deposits also known as Rossing-type or anatectic pegmatite- 34 alaskite deposits [1] currently provide approximately 10% of annual global uranium 35 production (6,400...
Alaskite - Definition, Usage & Quiz | UltimateLexicon.com
An in-depth look at Alaskite, its formation, geological characteristics, and its role in mineralogy. Discover the origins, uses, and notable occurrences of this intriguing granite variant.
Mechanisms of Formation of Alaskite, Aplite, and Pegmatite in a …
Examination of the relationships between textural variations and structural features in a complex, leucocratic dike swarm that is enclosed in the Half Dome quartz monzonite of the Sierra …
Petrology of the Alaskites of the Boulder Batholith, Montana
The alaskite occurs as dikes and as irregularly-shaped lenses or pods, primarily within the Butte quartz monsonite. Most of the contacts between the Butte quartz monzonite and alaskite are …
Alaskite: Mineral information, data and localities.
The term is used to designate granitoid rocks in which quartz constitutes 20% to 60% of the felsic minerals and in which the ratio of alkali feldspar to total feldspar is greater than 90%; i.e., the …
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