浙东南黄施岙钠长石岩石矿物学特征及矿床成因

栾进华; 高原; 徐厚倜; 杨仲可; 郑绪忠; 刘桂莲

doi:10.16152/j.cnki.xdxbzr.2024-03-017

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浙东南黄施岙钠长石岩石矿物学特征及矿床成因

地球科学 | 更新时间：2024-06-17

- 浙东南黄施岙钠长石岩石矿物学特征及矿床成因
- Mineralogical characteristics and genetic analysis of albite rocks in Huangshiao, southeastern Zhejiang
- 西北大学学报（自然科学版） 2024年54卷第3期页码：541-554
- 作者机构：
  
  1.重庆地质矿产研究院　重大地质事件资源环境效应重庆市重点实验室，重庆　401120
  2.重庆华地资环科技有限公司，重庆　401120
  3.浙江省第十一地质大队，浙江　温州　325006
- 作者简介：
  
  栾进华，男，正高级工程师，从事基础地质调查、矿产资源开发与研究，124407681@qq.com。
  高原，男，正高级工程师，从事矿床学与资源开发研究，49775907@qq.com。
- 基金信息：
  
  浙江省地质勘查基金项目(〔省资〕2023006);重庆市自然科学基金面上项目(CSTB2022NSCQ-MSX1375)
- DOI：10.16152/j.cnki.xdxbzr.2024-03-017
  中图分类号： P579; P611
- 纸质出版日期：2024-06-25，
  
  收稿日期：2023-12-19，
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栾进华, 高原, 徐厚倜, 等. 浙东南黄施岙钠长石岩石矿物学特征及矿床成因[J]. 西北大学学报（自然科学版）, 2024,54(3):541-554.

LUAN Jinhua, GAO Yuan, XU Houti, et al. Mineralogical characteristics and genetic analysis of albite rocks in Huangshiao, southeastern Zhejiang[J]. Journal of Northwest University (Natural Science Edition), 2024,54(3):541-554.
栾进华, 高原, 徐厚倜, 等. 浙东南黄施岙钠长石岩石矿物学特征及矿床成因[J]. 西北大学学报（自然科学版）, 2024,54(3):541-554. DOI： 10.16152/j.cnki.xdxbzr.2024-03-017.

LUAN Jinhua, GAO Yuan, XU Houti, et al. Mineralogical characteristics and genetic analysis of albite rocks in Huangshiao, southeastern Zhejiang[J]. Journal of Northwest University (Natural Science Edition), 2024,54(3):541-554. DOI： 10.16152/j.cnki.xdxbzr.2024-03-017.

摘要

通过对岩石化学、矿石结构构造、矿物组合特征等研究来分析浙东南黄施岙钠长石的岩石矿物学特征及矿床成因。研究认为，区内火山碎屑岩主要属酸性岩，岩石富碱(特别富钠)，贫钙、铁、镁，属钙碱性系列，为高钾型或普通型钙碱性岩石。钠长石岩矿床的形成与早白垩世火山活动有关，是中酸性的含矿热液交代富钠火山岩而成。矿床的分布与区域性深大断裂有关，受火山构造控制，富钠的中酸性岩类是有利成矿母岩，火山构造边缘的环形裂隙带以及不同岩相的接触带是有利的导矿、容矿构造，富钠岩浆提供热源和物源。矿床成因属火山(岩浆)热液蚀变型钠长石岩矿床。

Abstract

To explore the mineralogical characteristics and genesis of sodium feldspar by studying its petrochemistry

ore structure

and mineral combination characteristics. The volcanic clastic rocks in the area mainly belong to acidic rocks

which are rich in alkali (especially sodium) and poor in calcium

iron

and magnesium. They belong to the calcium alkaline series and are high potassium or ordinary calcium alkaline rocks. The formation of sodium feldspar deposits is related to early Cretaceous volcanic activity

where medium acidic ore bearing hydrothermal fluids were replaced by sodium rich volcanic rocks. The distribution of mineral deposits is related to regional deep and large faults

controlled by volcanic structures. Sodium rich acidic rocks are favorable ore-forming parent rocks. The circular fracture zones at the edge of volcanic structures and the contact zones of different rock facies are favorable ore conducting and hosting structures. Sodium rich magma provides heat and material sources. The genesis of the deposit belongs to the volcanic (magmatic) hydrothermal alteration type sodium feldspar deposit.

关键词

钠长石岩岩石化学矿物学矿床成因

Keywords

sodium feldspar rockpetrochemistrymineralogygenesis of mineral deposits

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