Xiaofei Zhang

Dr. Xiaofei Zhang


Research Focus & Metrics

Academic Career Length

3Years (2024-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
25 October 2024 in Lithos
Verified
Journal Article
Closed access
GCGuochao Chen
Guochao Chen
XZXiaofei Zhang
Xiaofei Zhang
XPXianzhi Pei
Xianzhi Pei
RLRuibao Li
Ruibao Li
ZLZuochen Li
Zuochen Li
RZRongzhen Zhang
Rongzhen Zhang

11 August 2026 in Minerals
Verified
Journal Article
Open access
PDF file
XZXiaofei Zhang
Xiaofei Zhang
JWJunlu Wang
Junlu Wang
HCHui Chen
Hui Chen
ZPZhenshan Pang
Zhenshan Pang
BYBing Yu
Bing Yu
XWXiatao Wu
Xiatao Wu
Amidst the intensification of strategic mineral exploration, the discovery of concealed and deep-seated deposits within covered areas and the peripheries of existing mines has become a critical challenge and a central focus of contemporary research. “Dongchuan-type” (DCT) copper deposits represent a key mineralization style within the SW Yangtze Block. However, significant exploration breakthroughs have stagnated over the past three decades. Consequently, advanced exploration prediction research is urgently required to guide deep-resource evaluation. Using the Shizishan copper deposit in the Yimen area as a representative case, this study applies the theory of “metallogenic geological body prediction” to construct a tripartite model encompassing “metallogenic geological bodies, metallogenic structures and structural planes, and metallogenic characteristic markers”. The Shizishan deposit is classified as a sedimentary-reformed type, characterized by multi-episodic mineralization involving initial sedimentary processes, non-magmatic hydrothermal activity, and subsequent structural-magmatic hydrothermal overprinting. Key metallogenic geological bodies include ore-bearing stratigraphic associations, basin-margin faults, NE-trending fold–fault systems, and deep-seated concealed intrusions. Metallogenic structural planes comprise primary ore-controlling surfaces, secondary fold-related structures, and potential deep-seated magmatic intrusive interfaces. Alteration patterns display a distinct vertical zonation: shallower levels show medium-to-low temperature hydrothermal processes (silicification, carbonatization, sericitization, and chloritization), whereas deeper portions reveal high-temperature magmatic–hydrothermal indicators, specifically skarnization and intense silicification. This study proposes that the integration of “stratigraphy + structures + concealed intrusions” should serve as the primary criterion for target screening in deep exploration. By integrating geophysical and geochemical datasets into this model, three promising exploration targets were delineated within the Yimen area. These findings provide a refined theoretical framework for large-scale prospecting of DCT.

1 January 2026 in Acta Petrologica Sinica
Verified
Journal Article
Open access
PDF file
XZXiaofei Zhang
Xiaofei Zhang
LCLuo Ci
Luo Ci
JWJunLu WANG
JunLu WANG
HCHui Chen
Hui Chen
ZPZhenShan PANG
ZhenShan PANG
GCGuoChao CHEN
GuoChao CHEN

镍、铬均为我国紧缺战略性矿产, 其资源安全保障风险突出, 亟需拓展国内找矿新区域、新类型。本次研究在西藏班公湖-怒江缝合带中段东巧地区首次系统评价了与沉积作用有关的镍铁(铬钴)资源。东巧地区发育与沉积作用相关的Ni、Fe、Cr、Co等多金属矿化, 主成矿元素Ni、Fe达到工业品位, 伴生元素Cr、Co可综合回收利用。矿(化)体主要赋存于下白垩统东巧组与超基性岩体的接触带部位, 其中东巧组下部碎屑岩中发育砂砾岩型、砂岩型镍铁(铬钴)矿, 超基性岩古风化层中发育风化型镍(钴)矿, 矿石矿物以含镍绿泥石、针铁矿、铬铁矿等为主。经系统评价, 新增推断资源量Ni金属量3.3万t, 伴生Cr2O3矿石量200余万t。矿石选冶实验表明, 采用"磁重选预富集铬资源-高压酸浸提取镍钴"的选冶联合工艺, 可满足该类型矿床开发利用要求。超基性岩古风化层及与蛇绿岩伴生的近源搬运再沉积地层是寻找该类型矿床的有利区。该发现突破了西藏地区仅在超基性岩内部寻找铬铁矿的局限, 拓展了我国镍矿、铬铁矿找矿新区域, 为Ni、Cr资源的勘探和开发提供了新的方向。