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程裕淇院士与鲁西早前寒武纪地质研究
引用本文:王世进,张增奇,杨恩秀,宋志勇.程裕淇院士与鲁西早前寒武纪地质研究[J].山东地质,2012(8):71-74.
作者姓名:王世进  张增奇  杨恩秀  宋志勇
作者单位:[1]山东省地质调查院,山东济南250013 [2]山东省地质科学实验研究院,山东济南250013
摘    要:程裕淇确定了泰山岩群雁翎关组、山草峪组、柳杭组地层划分,在斜长角闪岩中发现残存的变余杏仁状构造和岩流特征,正确区分了变基性熔岩流、变火山凝灰质岩和变基性脉体。原化马湾组黑云斜长片麻岩为新太古代早期条带状英云闪长质片麻岩。富山背斜的片麻状奥长花岗岩锆石SHRIMPU—Pb年龄(2612±20)Ma,其侵入的具变余气孔状充填构造的斜长角闪岩属于雁翎关组;而李家庄倒转向斜核部的柳杭组含砾黑云变粒岩中最年轻的碎屑锆石SHRIMPU—Pb年龄(2524±7)Ma。

关 键 词:程裕淇  研究成果  早前寒武纪地质  鲁西

CHENG Yuqi Academicians and Luxi Precambrian Geological Research
WANG Shijin,ZHANG Zengqi,YANG Enxiu,SONG Zhiyong.CHENG Yuqi Academicians and Luxi Precambrian Geological Research[J].Geology of Shandong,2012(8):71-74.
Authors:WANG Shijin  ZHANG Zengqi  YANG Enxiu  SONG Zhiyong
Institution:1. Shandong Geological Surveying Institute, Shandong Jinan 250013, China; 2. Shandong Institute and Laboratory of Geological Science, Shandong Jinan 250013, China)
Abstract:The division of Yanlingguan group, Shancaoyu group and Liuhang group in Taishan formation has been determined by CHENG Yuqi academician. Residual amygdaloidl structure and rock flow characteristics have been found in amphibolite, and meta--basic lava flow, meta--volcanic tuffaceous rocks and meta--basic veins have been correctly distinguished. Bearing biotite plagioclase gneiss in original Huamawan group is banded tonalite gneiss in early Archean period. SHRIMP U--Pb zircon age of gneissic trondhjemite in anticline of Fushan mountain is (2612 ± 20) Ma. Plagioclase amphibolites with vesicular filling structure belongs to Yanlingguan formation; while SHRIMP U--Pb age of the youngest fragements in gravel--bearing biotite leptynite in the core of Lijiazhuang inverted oblique in Liuhang group is (2524 ± 7) Ma.
Keywords:CHENG Yuqi  research achievements  Precambrian geology  Luxi area
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