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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第43卷

期数:

2021年第04期

页码:

643-660

栏目:

基础地质与矿产地质

出版日期:

2021-07-15

文章信息/Info

Title:

Diagenetic Sequence, Petrogenesis and Prospecting Prospect of Tangshe Complex Pluton in the Northeastern Margin of Jiangnan Orogenic Belt, China

文章编号:

1672-6561(2021)04-0643-18

作者:

张建芳; 蔡晓亮; 龚瑞君; 刘远栋; 王 振; 刘风龙; 汪隆武

(浙江省地质调查院,浙江 杭州 311203)

Author(s):

ZHANG Jian-fang;  CAI Xiao-liang;  GONG Rui-jun;  LIU Yuan-dong;  WANG Zhen;  LIU Feng-long;  WANG Long-wu

(Zhejiang Institute of Geological Survey, Hangzhou 311203, Zhejiang, China)

关键词:

地球化学;  岩石成因;  锆石U-Pb年龄;  成岩序列;  找矿前景;  复式岩体;  江南造山带

Keywords:

geochemistry;  petrogenesis;  zircon U-Pb age;  diagenetic sequence;  prospecting prospect;  complex pluton;  Jiangnan orogenic belt

分类号:

P581; P597; P617

DOI:

10.19814/j.jese.2020.07029

文献标志码:

A

摘要:

为了解江南造山带东北缘唐舍复式岩体成岩序列、岩石成因和找矿前景,采用区域地质填图、LA-ICP-MS锆石U-Pb定年和全岩地球化学特征分析等方法进行研究。野外地质接触关系厘定唐舍复式岩体的成岩序列为中粒二长花岗岩、中粗粒正长花岗岩、粗中粒斑状正长花岗岩和细粒正长花岗岩,锆石U-Pb年代学显示成岩时代分别为(140.4±3.3)、(131.7±3.2)、(132.2±1.6)和(125.0±2.0)Ma。各类岩石均具有高Si、富碱、低P、低Ti的特征,为准铝质—弱过铝质、高钾钙碱系列的I型花岗岩; 岩石的轻、重稀土元素分异程度较强,球粒陨石标准化稀土元素配分模式右倾,富集Rb、Th、U、K等,亏损Ba、Nb、Ta、Sr、P、Ti等,呈中等—强负Eu异常。总体上,唐舍复式岩体从早到晚岩浆演化具有SiO₂含量、K₂O含量、K₂O/Na₂O值、A/CNK值逐渐增高,TiO₂、Al₂O₃、TFeO、MgO、CaO、P₂O₅含量逐渐降低,负Eu异常逐渐增强,分异程度逐渐增高的趋势,为古太平洋板块俯冲-碰撞造山后陆内拉张环境下的下地壳物质重融,经结晶分异作用沿唐舍背斜构造侵位的产物。唐舍复式岩体侵入接触带由内向外矿化类型及矿种具有钨→银铅锌→锑/萤石的分带性,形成了一个矽卡岩型-热液脉型矿化系统,具有较好的找矿前景。

Abstract:

In order to understand the diagenetic sequence, petrogenesis and prospecting prospect of Tangshe complex pluton in the northeastern margin of Jiangnan orogenic belt, the regional geological mapping, LA-ICP-MS zircon U-Pb age, and all-rock geochemical analysis were studied. According to the geological contact relationship, the diagenetic sequence of Tangshe complex pluton from early to late is determined as medium grained monzonitic granite, medium-coarse grained syenogranite, coarse-medium grained porphyritic syenogranite and fine grained syenogranite, respectively, and the diagenetic ages are(140.4±3.3),(131.7±3.2),(132.2±1.6), and(125.0±2.0)Ma.The rocks have the characteristics of high Si and alkali, low P and Ti, being metaluminum-weak peraluminous and high-K calc-alkaline series, which belong to I-type granites. In addition, the light and heavy rare earth elements are highly differentiated, and the chrondrite-normalized REE pattern leans to right with the enrichment of Rb, Th, U, and K, the depletion of Ba, Nb, Ta, Sr, P, and Ti, and the medium-strong negative Eu anomaly. Generally, the magmatic evolution from early to late shows that the contents of SiO₂ and K₂O, the ratio of K₂O/Na₂O, and A/CNK gradually increase, the contents of TiO₂, Al₂O₃, TFeO, MgO, CaO, P₂O₅ gradually decrease, negative Eu anomaly gradually increases, and the degree of differentiation gradually increases. Tangshe complex pluton is the product of anticline tectonic emplacement after crystal-separation of the remelting of lower crustal material in the inland tension environment after the subduction-collision orogenic of paleo-Pacific plate.Types of mineralization and minerals in the contact zone of Tangshe complex pluton are characterized by W→Ag-Pb-Zn→Sb/fluorite zoning from inside to outside, which form a skarn-hydrothermal vein-type mineralization system with a good prospecting prospect.

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备注/Memo

备注/Memo:

收稿日期:2020-07-22; 修回日期:2020-10-25
基金项目:浙江省级地质专项资金项目([省资]2018006,[省资]2020005); 中国地质调查局地质调查项目(1212011220527,12120115030001)
作者简介:张建芳(1985-),男,福建浦城人,高级工程师,E-mail:zhjianfang@126.com。

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更新日期/Last Update: 2021-04-20