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Qingtian stone by the rhyolitic tuff and to open by the petrochemical kaolinite formed mainly used as printing stone, some also used for carving.

青田石系由流纹质凝灰岩经高岭石和地开石化而成,主要被用作印石,部分也用于工艺雕刻。

S: porous tuff ; rhyolitic vitric tuff ; porous material ; filter aids ; mineral material ; Quaternary

多孔凝灰岩;流纹质玻屑凝灰岩;多孔材料;助滤剂;矿物材料学;第四纪

From late Jurassic-early Cretaceous to late Cretaceous, the magmatic activities decrease and the compositions of magmas change from shoshonitic and rhyolitic to alkaline basaltic.

从晚侏罗世—早白垩世早期到晚白垩世,中国东部岩浆作用明显减弱,岩浆成分从钾玄质和流纹质向碱性玄武质转变。

Investigation results demonstrate that the age of intermediate to alkaline potash rich volcanic rocks of the first cycle of the Qingshan Formation is 109.9±0.6 Ma; and the age of the acidic rhyolitic volcanic rocks of the second cycle of the Qingshan Formation ...

结果表明,青山组第一旋回中偏碱性富钾火山岩的形成年龄为10 9.9± 0 。6Ma ,第二旋回酸性流纹质火山岩形成年龄为 10 8.2± 0 。6Ma ,据此确定胶莱盆地青山组火山岩应为早白垩世岩浆活动的产物。

Type I is composed of rhyolitic rocks, which are characterized by higher Si and alkali contents and lower Al and Ti contents, Na2O/K2O1 and a weak negative Eu anomaly (δEu=0.65–0.95), enriched in Sr and Ba and poor in Rb. Types I and II probably formed in an extensional to postorogenic extensional environment, accompanied by compressional uplift.

提要:大兴安岭北段根河地区早白垩世火山杂岩按岩石及其地球化学特征,可划分为3类:第Ⅰ类为流纹质岩石,富Si,碱,低Al,Ti,Na2O/K2O1,具弱的负Eu异常(δEu=0.65~0.95),富Sr,Ba,贫Rb;研究认为第Ⅰ,Ⅱ类岩石产于挤压隆升相伴的拉张至造山后伸展构造环境。

The studies on mineral geochemical for Erdaogou gold deposit located in the west part of Liaoning province indicate that it is characterized by low temperature mineral association such as pyrite, chalcopyrite, galena, sphalenite, telectrum, quartz, seriate, calcite, adual etc.

通过对二道沟金矿床矿物学的详细研究和对比,表明该矿床低温热液矿物组合和低温热液蚀变十分发育;与典型的冰长石-绢云母型浅成热液金矿的矿物组合十分相似;其应属于与流纹熔岩及其火山碎屑岩密切相关的浅成热液型金矿床

The original alkalic series of basalic magma evolutes into trachybasalt through crystallization differentiation of olivine and pyroxene, and the trachybasalt is transformed into alkalic rhyolite with remarkable Eu, Sr, Ba, Ti, P nagetive abnormalities through strong crystallization differentiation of plagioclase and also pyroxene Ti Fe oxides and apatite, all together leading to the loss of neutral (SiO 2=57%~63%) andesite and trachyandesite in the volcanic rocks in this area and appearance of bimodal volcanic rock combination feature.

原始碱性系列玄武质岩浆经橄榄石、辉石的结晶分异,向粗面玄武岩演化;粗面玄武岩经斜长石强烈的结晶分离作用,还有辉石、钛铁氧化物和磷灰石的分离结晶作用形成具显著Eu、Sr、Ba、Ti、P负异常的碱性流纹岩,导致本区火山岩缺失中性(SiO2=57%~63%)的安山岩和粗安岩,呈现双峰式火山岩组合的特点。

The Shengmikeng vein-type lead-zinc deposit is located in Huanggangshan volcano-tectonic depression of the Mesozoic volcanic belt in Northern Wuyi.The ore featured by veinlets and disseminations is hosted both inside the fault zone in the upper Jurassic Ehuling ignimbrite and the potassic trachyte porphyry.

摘 要:生米坑铅锌矿床位于北武夷中生代火山岩带的黄岗山火山盆地内,已知铅锌矿体呈脉状产于侏罗系上统鹅湖岭组流纹质熔结凝灰岩的断裂内,或呈细脉——浸染状分布于钾质粗面斑岩内,发育钾长石化、绿泥石化、硅化等蚀变。

The larvae gastropods T. riqueti were found abundantly in the four studying areas during October, and grew around a population of Ulothrix sp.

结果显示:小型腹足类-流纹绻之幼生,在秋季10月间会大量出现於三百多公倾之四大研究样区间,且混生於丝藻Ulothrix sp。

The volcanic rocks are dominated by basalts, diabases, andesite-basalts and with minor dacites and rhyolites, which are fallen into sub-alkaline series.

研究区内火山岩主要岩石类型为玄武岩、安山玄武岩、辉绿岩、安山岩以及少量英安岩和流纹岩。

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