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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。

The metal elements of the volcanic-hosted massive sulfide deposit have two sources, the copper and zinc are derived from rhyolitic magmas whereas the lead are probably related to old sediments overlying the rhyolites.(4) It is suggested here that the volcanic rocks hosting massive sulfide deposit in the north Qilian orogen, which are previously considered as a bimodal suite of Neo-proterozoic to middle Cambrian age in a continental rift, are virtually related to subduction magmatism in Ordovician age, and there might have no continental rift magmatism of Neo-proterozoic to middle Cambrian in the north Qilian.

Th/Ta比高(5.0~11.7),εNd为较大的负值(-2.6~-8.4),流纹岩的形成可能是两个端元组分混合的过程、或是上地壳混染的结果,形成在活动陆缘环境;(3)北祁连块状硫化物矿床成矿金属物质具有两种来源,Cu、Zn等来源于流纹岩,而Pb的来源可能与古老沉积物有关;(4)本文认为,前人厘定的北祁连新元古代-中寒武纪赋存块状硫化物矿床的大陆裂谷双峰式火山岩应是与俯冲作用有关的奥陶纪火山岩,说明北祁连可能不存在新元古代-中寒武纪的大陆裂谷活动。

Rhyolitic volcanic rocks are generally characterized by rich alkali, silicon, aluminum,and poor calcium, magnesium. They have relatively high Rb,Th and rather low Ba,Sr,Ti,P,and exhibit obviouslv negative europium anomaly (δEu=0.16~0.44).The εNd values of the rhyolitic volcanic rocks range from -5.93 to -2022.Basalts and rhyolites in different cycles show clear geochemical variance.

流纹质岩石总体具富碱、富硅、富铝,贫钙、贫镁特征,其Rb、Th等元素的含量较高,而Ba、Sr、Ti、P等元素含量则明显偏低,并具显著的铕负异常(εEu=0.16'0.44),岩石的εNd值变化于-5.93~~-2.22.I、II旋回玄武岩和流纹岩在地球化学特征上均具明显变异。

With high silica(SiO2 = 75.49 % on average), rich potassium(K2O = 3.88 % on average), low titanium (TiO2= 0.136% on average)and A/CNK high than 1.1(1.53 on average), the acidic volcanic rocks of Manghuai Formation belong to potassium-rich calc-alkali rhyolitic volcanic rock series.

官房地区火山岩属三江构造带南澜沧江构造岩浆带北段,中晚三叠世喷发了一套由中三叠统忙怀组酸性火山岩和上三叠统小定西组基性火山岩组成的火山岩系。

Geological and geochemical characteristics of the Early Ordovician volcanic rocks from North Qilian Mountain show that they are of the basalt-andesite association with no acid rocks or volcanic rocks of the shoshonite series.

早奥陶世阴沟群火山岩的地质-地球化学特征的研究结果表明,该期火山岩的岩石组合为玄武岩-安山岩组合,缺乏酸性火山岩和橄榄玄粗岩系列火山岩。

Mesozoic volcanic activities of the Tan Lu fault zone mainly appeared in Early Cretaceous and resulted in a set of volcanic rocks characterized by shoshonite series.

郯庐断裂带中生代火山活动主要发生在早白垩世,形成了一套以橄榄安粗岩系为主的火山岩。

Oligocene-Miocene volcanic rocks are shoshonite,late Miocene-Pleistocene volcanic rocks are High-k calc-alkaline.

渐新世-中新世火山岩以钾玄岩系列为主,部分为高钾碱性系列,火山活动强烈出露面积大而广泛。

Shoshonite ; high-K calc-alkaline ; volcanic cycle ; volcanic rocks Cenozic ; Hoh Xil Lake

钾玄岩系列;高钾钙碱性系列;火山旋回;新生代火山岩;可可西里湖地区

Studies of petrology and petrochemistry indicate that such suit of volcanic rocks dominated by lattite belongs to shoshonite series to potassic alkali basalt series. Considering the stability of rocks and their associations, gentle stratum occurrence, fresh degree of rocks and comparatively clarity of horizons. this potassic volcanic stratum distributed over the Sailipu area is named as Sailipu Formation, and the age of which is early middle Pleistocene of Quaternary.

岩石学、岩石化学研究表明,这套火山岩是以安粗质熔岩为主的钾玄岩系列-钾质碱性玄武岩系列火山岩,岩石类型及岩石组合稳定,岩层产状平缓,岩石新鲜,层位相对清楚,故将其命名为赛利普组,属第四纪早-中更新世。

The distinctive features of volcanic rocks, especially the spilite, illustrates that mantle plume or hotspot with small scale might be the essential origin of a series geologic events such as the extension of crust, the interval eruption of submarine bimodal volcanic rocks especially the increasing eruption of basic rocks, and the mineratlization of Ashele mine

认为成岩、成矿背景属裂陷拉张环境,火山岩尤其是细碧岩具有五大特殊性,初步提出了热点作用是导致地壳拉张、双峰式火山岩间互喷发、从早到晚基性火山作用趋于增强、以及成矿作用等一系列地质事件的深层次原因的看法

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