摘要
江西省东乡县大王桥－界头地段存在一套变质的超基性－基性－中酸性晶体堆积的侵入、喷出岩，其上为紊乱的海沟洋盆相、滨浅海相沉积岩，本文通过对该套岩石的分析，认为其为障公地体与怀玉地体缝合时形成的构造混杂岩体，初步确立了该古蛇绿岩套及混杂岩体。
There exists a suit of intrusive and extrusive rock accumalated bythe metamorphic ultrabasic-basic-intermediateacid crystals in Da-wangqiao-Jietou, Dongxiang county, Jiangxi province. Above it, tLereoccurs a disorder trench ocean basin facies and a shoreline marine sedi-nentary rock. Through an analysis of the suit of rock, the authorsiold that it is a tectonic mixtite body formed as a result of Zhanggong terrance and Huaiyu terrance being sutured. Therefore, the ophio-tite suit and the mixite body were preliminaryly determined.
出处
《江西地质》
1995年第3期177-186,共10页
Jiangxi Geology
