Earth Science Frontiers ›› 2021, Vol. 28 ›› Issue (1): 363-374.DOI: 10.13745/j.esf.sf.2020.11.11

Previous Articles     Next Articles

Geochemical genes related to granite weathering in the Yunmengshan area of Beijing, China

WANG Xuyang(), YAO Ning, GONG Qingjie*(), CHAO Yuede, PENG Cheng, WU Yuan   

  1. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China
  • Received:2019-12-05 Revised:2020-11-25 Online:2021-01-25 Published:2021-01-28
  • Contact: GONG Qingjie

Abstract:

The geochemical gene technique is a new geochemical tracing technique formally proposed over the past two years. In this investigation, samples from two adjacent weathering profiles (B and C) developed in granite in the Yunmengshan area of Beijing, China were collected to test two geochemical genes named lithogene and gold metallogene. In samples from profile B, the chemical index of alteration (CIA) varied between 51.3-58.9, and the weathering index of granite (WIG) varied between 68.6-89.4, indicating incipient weathering in this profile; while in samples from profile C, CIA varied between 52.4-78.4, and WIG between 25.3-84.8, indicating intermediate weathering in profile C. The noticeable difference of weathering degrees between the two adjacent profiles indicates that different micro-environment may result in significantly different weathering products in the same granite. The lithogene similarity between samples and fresh granite varied from 85% to 100% in profile B and 90% to 100% in profile C, while the gold metallogene similarity between the two varied from 85% to 100% in profile B and 80% to 100% in profile C. With respect to top soil, the similarity of lithogenes varied from 80% to 100% in profile B and 90% to 100% in profile C, and the gold metallogene similarity varied from 85% to 100% in profile B and 80% to 100% in profile C. According to the criterion that gene similarity above 80% indicates similar genes, the lithogene and gold metallogene illustrate not only good heredity and inheritance in each profile but also high similarity between the two profiles. Besides, with respect to the ideal gold ore (gold metallogene 12020202020), the similarity of gold metallogenes varied from 25% to 50% in profile B and 30% to 50% in profile C. According to the criterion that mineralization can be recognized when the gold metallogene similarity reaches 40%, one mineralization layer of ca. 1 m thickness can be recognized in each profile. Thus, the gold metallogene may also be used as an integrated geochemical indicator in gold exploration.

Key words: weathering profiles of granite, geochemical lithogene, geochemical gold metallogene, weathering indices, micro-environment

CLC Number: