1.
Studies of Mafic and Ultramafic Rocks Along the Shang-Dan Suture from Qinling Orogenic Belt and Their Implications;
秦岭商—丹构造带镁铁质、超镁铁质岩体研究及其地质意义
2.
There are over 30 mafic and ultramafic intrusions in the area and Cu-Ni sulfide ore bodies were found in No. 1 and No. 7 ultramafic intrusive bodies which exhibit obvious zoning and cumulate texture.
区内出露30多个镁铁－超镁铁质岩体，其中1、7号超镁铁岩体中赋存铜镍硫化物矿（床）体。
3.
Petrogenesis of Kalatongke mafic rock intrusions, Xinjiang.
新疆喀拉通克镁铁质岩体群的岩石成因研究
4.
The ore-forming geological features and prospecting significance of mafic and ultramafic intrusions in Sandaogang area,Panshi City Jilin Province
吉林磐石市三道岗镁铁—超镁铁质岩体成矿地质特征及找矿意义
5.
GEOLOGIC CHARACTERISTICS AND PROSPECTING GUIDE OF THE MAFIC-ULTRAMAFIC INTRUSIVE BODIES IN CHAJIAN ORE DISTRICT,JILIN PROVINCE
吉林省茶尖矿区镁铁-超镁铁质岩体地质特征及找矿方向
6.
Geochemistry and Chronology of Ultramafites from the Songshugou Area in Qinling;
秦岭松树沟超镁铁质岩体地球化学及年代学
7.
LA-ICP-MS zircon dating from the Lajimiao mafic complex in the Qinling orogenic belt
秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究
8.
Geochemistry and petrogenesis of Xingdi No. 2 mafic-ultramafic intrusion in the Kuluketag area, Xinjiang
新疆库鲁克塔格地区兴地Ⅱ号镁铁-超镁铁质岩体的地球化学特征与岩石成因
9.
Characteristics of zircons from a metamorphic contact zone of the Songshugou ultramafic pluton in North Qinling and their geological significance
北秦岭松树沟超镁铁质岩体接触变质带中锆石特征及其地质意义
10.
Owing to ultramafites coming from mantle, it contains abundant deep information of geology.
超镁铁质岩体由于来自地幔,而含有丰富的深部地质信息。
11.
The rock-body which have the relation of mtallogenic of copper-nickel ore have the characteristic of compound rock-body. They belong to mafic, ultramafic rocks which type are gabbro, pyroxenite and peridotite.
与铜镍矿成矿有关的岩体具有复合杂岩体特征,多属辉长岩—辉石岩—橄榄岩型镁铁—超镁铁质岩。
12.
Petrogenesis and Magma Source of the Mafic-ultramafic Complex in the Northeast of Tarim Plate;
塔里木板块东北部二叠纪镁铁质—超镁铁质杂岩体成因
13.
Geochemistry of Sifangtai Mafic-ultramafic Complex,and Its Tectonic Implications;
四方台镁铁—超镁铁质杂岩体的地球化学特征及其大地构造意义
14.
The protolith of Bixiling garnet peridotite-eclogite massif in Dabie Mountains, China is a mafic-ultramafic intrusive body, which was formed in an island-arc environment and subjected to crystallizationfractionation.
碧溪岭橄榄岩一榴辉岩体的原岩为形成于岛弧环境并经受结晶分离作用的镁铁－镁铁质侵入体。
15.
Zircon SHRIMP U-Pb dating of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei Province, China.
河北矾山钾质碱性超镁铁岩-正长岩杂岩体的锆石SHRIMP U-Pb年龄
16.
Discovery of komatiitic ultramafic intrusion in Mid-Tianshan terrain; Xiadong intrusion, Xinjiang.
中天山地块科马提质超镁铁岩体的发现:新疆峡东岩体
17.
FEATURES AND MEANING OF MAFIC MICROGRANULAR ENCLAVE IN XIAERPU GRANITE IN WEST JUNGGAR,XINJIANG
新疆西准噶尔夏尔莆岩体中微粒镁铁质包体特征及意义
18.
The Mafic-ultramafic Intrusions in the Huangshan Region Eastern Tianshan, Xinjiang: Petrogenesis and Mineralization Implication
新疆东天山黄山岩带镁铁—超镁铁质岩石成因及成矿作用