Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物主要地表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

主要类质同象存在于闪锌矿中,少量矿等独立矿物式存在于矿床的氧化带，是风化淋滤过程中成的的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚部为风化淋滤富集成。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物主要为地表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

主要以类质同象存于闪锌中,少量以等独立物式存于床的氧化带，是风化淋滤过程中成的的次生物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期浅部为风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物主要为地表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象于闪锌矿中,少量镉以硫镉矿等独立矿物于矿床的氧化带，是风化淋滤过程中成的镉的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在浅部为风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩带位风化壳表层上部，风化淋滤及表径流改造而破碎，短距离搬运堆积相对较低的风化壳表面，成一些沟、洞、缝、蚀、蚀漏斗及落水洞等，其充填物主要为表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在闪锌矿中,少量镉以硫镉矿等独立矿物式存在矿床的氧化带，是风化淋滤过程中成的镉的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在浅部为风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

岩溶带位于风化壳部，风化淋滤及地径流改造而破碎，短距离搬运堆于地势相对较低洼的风化壳面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物主要为地残物和洞物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在于闪锌矿中,少量镉以硫镉矿等独立矿物式存在于矿床的氧化带，是风化淋滤过程中成的镉的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在浅部为风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而，距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶、溶缝、溶蚀洼地、溶蚀漏斗及落水，充填物主要为地表残积物和壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在于闪锌矿中,少量镉以硫镉矿独立矿物式存在于矿床的氧化带，是风化淋滤过程中成的镉的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

期在浅部为风化淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞，其充填物主要为地表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在于闪锌矿中,少量镉以硫镉矿矿物式存在于矿床的氧化带，是风化淋滤过程中成的镉的次生矿物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在浅部为风化淋滤富集成。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼的风化壳表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物主要为地表残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在于闪锌中,少量镉以硫镉等物式存在于床的氧化带，是风化淋滤过程中成的镉的次生物。

Many diorite porphyrite and albite aplite dikes are found in the gold district and its surrounding areas.

晚期在浅部为风淋滤富集成矿。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

层岩带位于风层上部，风淋滤及地径流改造而破碎，短距离搬运堆积于地势相对较低洼的风面，成沟、洞、缝、蚀洼地、蚀漏斗及落水洞等，其充填物主要为地残积物和洞壁塌积物。

There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.

镉主要以类质同象存在于闪锌矿中,少量镉以硫镉矿等独立矿物式存在于矿床的氧带，是风淋滤过程中成的镉的次生矿物。