1.Evidence of emergence including sabkha dolostone, algal mat, bird-eyes and fenestral structure, mudcracks and crustose limonite has been found in the top of the Changhsingian reefs in Ziyun, Guizhou province.
贵州紫云长兴期生物礁顶部存在的出露证据有：（1）形成于萨勃哈蒸发环境的白云岩，（2）藻纹层沉积，（3）鸟眼和窗格构造，（4）干裂缝和褐铁矿风化壳，等等。
2.The Banhua stone as a decoeration pigment is a kind of limonite which could be transferred to hematite α-Fe_2O_3 and magnetite in the heating process, so the porcelain surface was covered with black or brown design deeoration.
斑花石是一种作为颜料用的褐铁矿,在加?峁?讨兴?嶙?湮?痢?e_2O_3赤铁矿和磁铁矿,以使瓷器表面产生黑色或褐色花纹。
3.Glauconite, hematite-limonite and some chlorite are formed in syndiagenesis.
形成于同生成岩期的自生矿物有海绿石，赤铁矿～褐铁矿和部分绿泥石。
4.Huangmei has a rich reserve of underground minerals, 15 sorts are proven to have exploitation value, of which, limonite and siderite have a reserve of 58 million tons, the tenor is around 45%, being concentrated; quartz is of 100 million tons; gypsum mine is 270 million tons; barite is 500,000 tons and silex of 10 million tons; porcelain clay, limestone, shale and granite are extensively distributed and of large reserve.
黄梅地下矿产丰富,已探明有开采价值的矿产资源15种,其中褐铁矿、菱铁矿储量5800万吨,品位45%左右,分布集中；石英矿1亿吨；石膏矿2.7亿吨；重晶石50万吨；硅石1000万吨；瓷土、石灰石、页岩石、花岗岩分布广、储量大。
5.Study on direct heap leaching of gold-bearing limonite ore
含金褐铁矿直接堆浸的初步探讨
6.Isotopic chronological study of mineralization show that the fluid inclusion Rb-Sr isochron age for gold-bearing pyrite-quartz veins and pyrite-limonite-quartz veins from the Dashankou gold mine are 354±8.1Ma (2σ ) and 344±21Ma (2σ ), respectively. The two ages are consistent in test errors, indicating the gold deposit was formed in early Carboniferous and related to regional shearing;
成矿作用同位素地质年代学研究表明,大山口金矿区含金黄铁矿—石英脉和含金黄铁矿—褐铁矿—石英脉的石英流体包裹体Rb—Sr等时线年龄分别为354±8.1Ma(2σ)和344±21Ma(2σ),两者在实验测定误差范围内一致,代表大山口金矿形成的时间发生于早石炭世,成矿作用与区域韧性剪切作用有关;
7.pigment consisting of a limonite mixed with clay and silica.
由褐铁矿与粘土、硅土混合而成的颜料。
