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

晚期在浅部为化淋滤富集成矿。

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

表层岩溶带化壳表层上部，化淋滤及地表径流改造而破碎，短距离搬运堆积地势相对较低洼的化壳表面，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.

镉类质同象存在闪锌矿中,少量镉硫镉矿等独立矿物式存在矿床的氧化带，是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.

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，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,少量镉以硫镉立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.

晚期浅部为风化淋滤富。

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

表层岩溶带位风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积地势相对较低洼的风化壳表面，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锌中,少量镉以硫镉等独立物式存床的氧化带，是风化淋滤过程中的镉的次生物。

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，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，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.

晚期在浅部为风化富集成矿。

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

层岩溶带位于风化壳层上部，风化地径流改造而破碎，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、溶蚀漏斗落水洞等，其充填物主要为地物和洞壁塌物。

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，风化淋滤及地表径流改造而破碎，短距离搬运地势相对较低洼的风化壳表面，成一些沟、洞、缝、洼地、斗及落水洞等，其充填物主要为地表残物和洞壁塌物。

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的表面，成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填要为地表残积和洞壁塌积。

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.

要以类质同象存在于闪锌矿中,少量以硫矿等独立矿式存在于矿床的氧带，是淋滤过程中成的的次生矿。

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，其主要为地表残积和洞壁塌积。

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。

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，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，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。