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，风化淋滤地表径流改造而破碎，短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.

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.

镉主要以类质同象在于闪锌矿中,少量镉以硫镉矿等独立矿物在于矿床的氧化带，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低洼的风化壳表面，成一些沟、洞、、洼地、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中,少量镉以硫镉等独立物式存在于床的氧化带，是风化淋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.

表层岩带位于壳表层上部，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壳表面，成一些、洞、缝、蚀洼地、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矿中,少量镉以硫镉矿等独立矿物式存在于矿床氧带，是淋滤过程中成镉次生矿物。

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，风化淋滤地表径流改造而破碎，短距离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低洼的风化壳表面，成一些沟、洞、、洼地、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。