orebody

The orebody take the shape of prolate lenticle and appearing horizontal bedding.

区内有优质的硅藻土及硅藻粘土级矿石。

The orebodies occur within or near the exocontact of intrusive rocks and above the hidden igneous rocks.

金矿产于体外接触及其附近和隐伏体上方。

The ore-bearing beds have a bimodal rock association and exhibit assembly characteristics of pyroclastic rock, orebody and exhalite.

含矿系为双峰石组合，具有火山碎屑-矿体-喷气“三位一体”特徵。

Orebodies in sedirmentary rock hosted Au deposits are discrete hypogene and epigenetic masses usually hosted in a fault zone, breccia mass, or lithologic bed or unit.

沉积金矿床的矿体是一些不连续的内或后地质体,通常赋存于断裂、角砾体或层(性单位)中。

There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

构造破碎的石具有明显的对称分性：破碎的中心为钠柱石矿体，向侧依次为榍石透辉石长英、黑云母钠长，逐渐过渡为围。钠柱石矿的成因类型为沿构造破碎产出的热液交代脉型。

The study shows that the gold quartz vein is the largest orebody which was controlled by E-W extrusion fracture zone.The kaligranite and spessartite are the largest wallrocks.

研究表明大庙子—板庙子金矿化区内金矿体以石英脉型为主,矿体的产出受东西向挤压破碎控制,钾质花岗和闪斜煌斑是矿体的主要围;

Gold quartz vein is the major orebody which is controlled by E-W-extrusion fracture zone in the Damiaozi gold mineralized district.The granite-porphyry,spessartite and diabase are the major wallrock.

大庙子金矿化区内金矿体以石英脉型为主,矿体的产出受东西向挤压破碎控制,花岗斑和闪斜煌斑、辉绿是矿体的主要围。

Copper mineral belts can be easily seen in orebody.There has clear border between footwall and base of orebody, but it changes gradually from ore to its hangingwall.

铜矿化具有明显的分特征,矿体底板与围之间界限清楚,顶板与围之间呈渐变过渡;

The orebody is controlled by SN, NW faults and fissures, the ore deposit belongs to magmatic hydrothermalism-stratabound and compound magmatic hydrothermalism type one.

矿体受南北向、北西向断裂及裂隙构造控制,矿床成因为浆热液—层控与浆热液复合型。