1) Jinning
晋宁
1.
In this paper,the characteristics and intluence factors of Jinning P deposit and(the correct) discriminance of weathered ore are put forward according to the composition and structure alteration of phosphorite in the weathering process of P ore.
根据晋宁磷矿次生风化作用过程中磷块岩组成和结构的变化 ,归纳晋宁磷矿矿床特征及其影响因素 ,正确确定该矿风化矿石的判别指标。
2.
The Jinning Anning area is the most famous phosphorite producing area in China.
晋宁、安宁地区中谊村段的白泥层与中白云岩层为上下关系，中白云岩层为上磷矿层下部的相变。
2) Jinningian
晋宁期
1.
Geochemical Features and Its Tectonic Implication of the Jinningian Wangjiangshan Gabbros in the North Margin of Yangtze Block;
扬子北缘晋宁期望江山基性岩体的地球化学特征及其构造背景
2.
The result showed that the minerogenetic age is Jinningian (784 Ma).
地质特征研究表明:该矿床后期改造作用明显,并非同生沉积或成岩作用早期成矿,而与晋宁期Rodina大陆裂解有关。
3.
In fact,the deposit did not belong to idiogenous sedimentation or formed in early stage of diagenesis and the mineralization was related with the Jinningian break-up of Rodinia.
该矿床后期改造作用明显,并非同生沉积或成岩作用早期成矿,而与晋宁期Rodina大陆裂解有关。
3) Pre-Jinning
前晋宁期
1.
Many Pre-Jinning layered intrusions in Pre-Sinian bsement complex are occurred in Panxi area,in which V-Ti magnetite and chromite mineralizations can be found.
攀西地区大片前震旦纪结晶基底杂岩中产出有众多的前晋宁期层状侵入体 ,其间可见钒钛磁铁矿化 ,铬铁矿化。
4) Jinning period
晋宁期
1.
The metamorphic rocks formed in Jinning period in Zhenghe area, northern Fujian province, encountered four times of complex deformations.
政和地区变质岩石形成于晋宁期,遭受了四期复杂的构造变形作用。
5) Ningjinpo Lake
宁晋泊
1.
Evolution of Daluze and Ningjinpo Lakes in Southern Part of the Haihe River Valley since the Ming Dynasty;
明代以来大陆泽与宁晋泊的演变过程
6) Jinning epoch
晋宁期
1.
Discovery and geological significance of metamorphic and intrusive rock (system) of Qimantage region in Jinning epoch;
祁漫塔格地区晋宁期变质侵入岩(体)的发现及其地质意义
补充资料：晋宁感兴
【诗文】：
莫将官况说葭芦，一味萧条称鄙夫。
老圃不禁蔬代肉，樵丁还喜炕连厨。
儿音半已渐秦晋，乡信无因接鲁洙。
三见秋风落庭树，年年归意负莼鲈。
【注释】：
【出处】：
莫将官况说葭芦，一味萧条称鄙夫。
老圃不禁蔬代肉，樵丁还喜炕连厨。
儿音半已渐秦晋，乡信无因接鲁洙。
三见秋风落庭树，年年归意负莼鲈。
【注释】：
【出处】：
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条