华南地质与矿产
華南地質與礦產
화남지질여광산
GEOLOGY AND MINERAL RESOURCES OF SOUTH CHINA
2014年
4期
308-318
,共11页
牛志军%杨文强%刘浩%宋芳
牛誌軍%楊文彊%劉浩%宋芳
우지군%양문강%류호%송방
南岭成矿带%青白口系%南华系%震旦系
南嶺成礦帶%青白口繫%南華繫%震旦繫
남령성광대%청백구계%남화계%진단계
Qingbaikouan System%Nanhuan System%Sinian System%Nanling Metallogenic Belt
南岭成矿带前寒武系为金、铁、锰、磷及铅锌的赋矿层位,近年来由于高精度测年数据的应用,建立了较为清晰的年代地层格架,然而由于历史原因,前寒武系岩石地层序列在湘黔桂赣粤交界地区存在同物异名现象,不利于地质矿产图的编制,需要重新厘定完善。本文以武陵运动构造面为界,将南岭成矿带大地构造演化分为两个阶段,按中元古代至青白口纪早期、青白口纪晚期至震旦纪划分出不同地层区。早期划分出两个地层区—扬子与华夏地层区,晚期同属于华南地层区,依据处于盆地不同位置,再划分为六个地层分区。本文重点对湘黔桂交界地区的青白口系上部层位、赣湘桂地区南华系和震旦系进行了梳理,初步形成前寒武纪岩石地层序列,不再采用部分岩石地层单位,以便于编制该地区地质矿产图。
南嶺成礦帶前寒武繫為金、鐵、錳、燐及鉛鋅的賦礦層位,近年來由于高精度測年數據的應用,建立瞭較為清晰的年代地層格架,然而由于歷史原因,前寒武繫巖石地層序列在湘黔桂贛粵交界地區存在同物異名現象,不利于地質礦產圖的編製,需要重新釐定完善。本文以武陵運動構造麵為界,將南嶺成礦帶大地構造縯化分為兩箇階段,按中元古代至青白口紀早期、青白口紀晚期至震旦紀劃分齣不同地層區。早期劃分齣兩箇地層區—颺子與華夏地層區,晚期同屬于華南地層區,依據處于盆地不同位置,再劃分為六箇地層分區。本文重點對湘黔桂交界地區的青白口繫上部層位、贛湘桂地區南華繫和震旦繫進行瞭梳理,初步形成前寒武紀巖石地層序列,不再採用部分巖石地層單位,以便于編製該地區地質礦產圖。
남령성광대전한무계위금、철、맹、린급연자적부광층위,근년래유우고정도측년수거적응용,건립료교위청석적년대지층격가,연이유우역사원인,전한무계암석지층서렬재상검계공월교계지구존재동물이명현상,불리우지질광산도적편제,수요중신전정완선。본문이무릉운동구조면위계,장남령성광대대지구조연화분위량개계단,안중원고대지청백구기조기、청백구기만기지진단기화분출불동지층구。조기화분출량개지층구—양자여화하지층구,만기동속우화남지층구,의거처우분지불동위치,재화분위륙개지층분구。본문중점대상검계교계지구적청백구계상부층위、공상계지구남화계화진단계진행료소리,초보형성전한무기암석지층서렬,불재채용부분암석지층단위,이편우편제해지구지질광산도。
Precambrian system in Nanling Metallogenic Belt is the layer of occurrence of gold, iron, manganese, phosphorus, and lead & zinc. Chronostratigraphic framework has been well-grounded redefined, based on publi-cation of a series of high accuracy dating data. Meanwhile, synonyms, which have negative effects on geological mapping, still occur in stratigraphic sequences of Precambrian System of the area, and that should be elaborately redefined. In this paper, stratigraphic regionalization of Mesoprotozoic to early Qingbaikouan and late Qingbaik-ouan to Sinian in Nanling Metallogenic Belt differ on the basis of two stages of tectonic evolution, which could be divided by angular unconformity between Lengjiaxi and Banxi Groups, generated by Wuling Orogeny. Early stage is divided into Yangtze and Cathaysian stratigraphic regions; and the late into six stratigraphic sub-regions, all of which belong to South China region, according to their different locations in the depression. The paper focuses on teasing out the upper part of Qingbaikouan System in borderland of Hunan, Guizhou and Guangxi, together with Nanhua to Sinian Systems in Jiangxi, Hunan and Guangxi, abolishing some lithostratigraphic units’names, in or-der to develop uniform standard of lithostratigraphic sequences in convenience of geological mapping of this area.