Granite contain mine exclusive attribute analysis

Nina

December 29, 2022 at 7:40 pm

The research zone is located in the Yichun -Yanshou Non -Metal Mine and Iron Mine Mining Ambuers (Han Zhenxin et al., 2004), the most important lead, zinc, iron, tungsten, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, and molybdenum, Waiting for a multi -metal symbiotic convergence zone. The invasive rock is widely revealed in this area, and its relationship with minerals is more closely related to minerals. It is mainly tungsten, molybdenum, lead, zinc, and iron mineral (points).
1. Ancient Yuan and ancient granite
The ancient crystal base in the research area Xingdong Rock Group and the iron rock layer in the Dongfeng Mountain Rock Group were invaded by regional deterioration and granite sage hemp rocks -under the action of thermal fluid Once again, the East Wind Magnetic quartz -type iron ore is formed.
The ancient Yuan Granite Film Miscellaneous Rock (PT1GN) is compared with the granite hemp rocks of the Grandma Miscellaneous Rock in Xing'an -Jihei Zengshan Belt in Inner Mongolia (Chi Qinghua et al., 2007). PB, SN enrichment, ZN, CR, NI and other elements have decreased, and the MO content is similar (Table 5-2). The relationship between the ancient Yuan ancient granite tablets and the gold mineralization of the ancient Yuan Gang is closely related. The average AU content of the ancient granite tablets hemp rock was 0.05 × 10-6 (Han Zhenxin et al., 2004). It can be speculated that the ancient crystal base rock is one of the mineral rocks of rock gold and sand gold. Jinfeng's value has significantly reduced its gold content from the ancient base metamorphic rock → granite sliced hemp rock (granite), indicating that the gold with granite is migrated, and the hot liquid gold mine may be formed under the right conditions. Essence In this work, in the ancient Yuan and ancient granite tablets of the Songlin Forest Farm of Xinqing Forestry Bureau, three new rock gold mineralized body was found in the deterioration of the metamorphic layers of the Dongfeng Mountains. Therefore, pay attention to finding rock gold mines in the ancient crystal base.
2. The ancient granite of the Chinese and premium
is mainly ultra-magnesium-iron magnesium miscellaneous rocks, which are produced with rock-shaped output. In the rock group, the high -voltage blue rock phase with Heilongjiang Rocks -deep -pressure green sliced rock -like deep -sea silicon deposits, medium base sea rock rocks, etc., constitute the ancient Taipinggou -Golden Mine Forest Snake Green Rock Set ( Cao Yan et al., 1992; Qiqihar Branch, Heilongjiang Province, 2006). Miscellaneous rocks are composed of snake -grained rocks, penetrating glitter rocks, and green mud rock rocks. The content of trace elements CR, Ni, and CO of rocks is very high, and it is 2010 × 10-6 to 2600 × 10-6, 1340 × 10-6 ～ 1860 × 10-6, 59.7 × 10-6 ～ 83.8 × 10-6 (Table), its magma comes from the source of the mantle. They have a cause of contact with the minerals, which can be CR, Ni, and CO ore sources. Compared with the ultra-magnesium iron rock in the eastern part of China (Chi Qinghua et al., 2007), the content of CU, PB, Zn, AU, SB is reduced, the MO content is similar, and the rich SN element is characterized (Table 5-2).
Thetegly granite trace element content in different times of the research area of different times of the research area
If in the ancient Jiamusi plot in the stretch structure environment to form a small ocean basin During the collage, the magnesium iron quality -ultra -magnesium iron miscellaneous rock was broken in the reducing zone, and then the characteristics of linear beadin -like distribution were broken along the backbuilding or sliding break -off fault, which explained China -Yuan ancient snake green rocks (magnesium iron -ultra -magnesium iron miscellaneous rocks) constructed constructive invasion of collage collage collaboration collaboration -arc land collage and make them mutually collage hyperplasia, becoming the ancient and hyperplasia of China Part of the band.
3. Gali East Period granite
This granite is near SN to the band to the band of Yichun -Yanshou fold system and Xingkai Lake -Lao Lingling plot. That is, near the west side of the Mudanjiang Deep Fracture Belt. The granite ingredients have changed greatly in this period. From early to late rock types, the type of lithography has evolved from quartz glittering long rocks → granite flashes long rock → second -long granite. The type of rock type evolved from neutral → acidity. It is a relatively complete sequence of component evolution. In the wild macro, different ingredients of rocks are interspersed with each other, wrapped and gradient contact relationships. In advanced rock body, magma mixing the cause of magma mixed with the MME type microclican long -quality bag, which has a significant shell mixture mixed rock phase learning. , Rock Chemical, Earth Chemical characteristics. The rock body is formed in the edge environment of the continental curved activity of the land edge, which may represent the collapse of the collage between the collage between the combination and collage between the Jiamusi plot between the Jiamusi plot in the early ancient generation. The shell mantle mixed effect (Han Zhenzhe et al., 2009B) under the influence of the bottom invasion, which has broaden ideas for the research of Gali East Period granite in the region.
The trace elements in the second long granite of the Gali East phase comparison with the average value of the two long granite with the second long granite of the Xing'an -Jihei Crream Mountains in Inner Mongolia (Chi Qinghua et al., 2007), CU, PB, Zn, MO, W, SN and other elements are enriched. The content of AU and AG is low (Table 5-2), and elements such as CU, PB, Zn, MO, SN in Government Flashing and Flashing rocks are also rich. This issue is closely related to PB, Zn, W, MO, and Fe mineralization, which constitutes the first period of the first phase of Yichun -Yanshou Nonferrous Metal and Iron Mine Mine. The important heat source of contact type and thermal liquid minerals in China.
Ilin (super) large lead zinc mine and iron multi -metal mineral beds are related to typical mines related to Gali East period granite. Similar, and the PB isotope composition of the sedimentary rock sedimentation of the lead mountain group is relatively large, reflected in minerals mainly from magma (Han Zhenxin et al., 2004), indicating that the source of the magma may be rich in PB, Zn, etc. In the process, further extension with magnesium -rich carbonate surrounding rocks, drawing the mineral division in the surrounding rock, and with the differentiation of the magma, the mining group is continuously enriched in the magma, lead zinc zinc, and lead zinc zinc Minerization is a large amount of precipitation in accordance with the filling and explanation method, forming a low -temperature heat -charging -contact -type lead -zinc mine.
4. Huali West Period granite
This in the middle of Huali West in the middle of Huali West, anesthetic medium granules (ring spots) two long granite invading the Dali of the East Fengshan Rock in the ancient Yuan Dynasty, forming Silicon stroke -type groups of iron ore, Golden River zinc iron ore, field cannon lead zinc ore point, etc. The ore body is mainly produced in the internal and external contact zone, and a few are produced in the second -long granite of the eclipse. The weak sliced siber -like medium granules (ring spots) and the two -long granite invaded the lead mountain group of the Cambrian Xilin group under the Silicon Calcium Rock type Xiying Iron Mineralization Point. Dali rocks in the Ling Group form a large Kunlun iron ore filled with a Silicon Calcium type -thermal fluid. In summary, when Huali West invades rocks into the above -mentioned strata, the invasive contact belts are invaded and formed to form horny, silicon blocons, and mineralization such as iron, lead, and zinc. type. In the northern Dabao Mountain area of Xiaoxing'an Ling, Hualili West Period granite is closely related to CU, MO, AU, and FE, and has a strong mineral effect (Du Qi, 1988).
It -shaped siber -shaped medium grains like spots (ring spots) two long granite, granite flashes long rocks and other rocks with the average value of the two long granite in Inner Mongolia -Jihei Creation Mountain (Chi Qinghua et al., 2007), CU, CU, CU, CU, CU, CU, ZN, MO, W, SN and other elements are enriched. PB and AG have basically no change, while AU, NI and other elements are poor (Table 5-2), indicating that the rocks may be multi-metal CU, Zn, MO, W, Sn, etc. One of the mineral rocks of mineral elements. In addition, it is worth mentioning that the content of mineral elements such as CU, Zn, MO, etc. in the fine -grained long quality bag is significantly higher than that of the host rock (Han Zhenzhe et al., 2008A), implying that there are many iron, more iron, more iron and more in the southeast of Xiaoxing'an Ridge. Metal beds are closely related to the mixing effect of magma, which may be related to the ore elements such as CU, MO, PB, Zn, FE, and other mineral elements.
5. Indiacopy Period granite
This granite invasion in this issue is strong, which is one of the main heat sources of Xiaoxing'an Ridge -Zhangguangcai Laoling Metal Mining Belt One of the mineral rocks. The dewy is mainly based on the combination of spots -like two -long granite. This issue of granite is the key research object of this book. Its detailed rock science, main trace, isotope, and the characteristics of mineralization are shown in the third and fourth primary chapters.
The comparison with the average value of the two long granite in Inner Mongolia -Jihei Building Mountain with two long granite (Chi Qinghua et al., 2007), CU, Zn, MO, W, SN and other elements in the spots are rich. The PB content is close, and AG is slightly poor. Among them, the fine-grained giant spots-like two-long granite CU and W are the most enriched. The CU value is as high as 144.3 × 10-6, which is dozens of times higher. The granite is the highest, up to 2.6 × 10-6, more than several times high, and W is also the highest in the giant giant spots in the fine-grained giant spots. In the long-alkali-long granite, W and MOs are the most enriched. The elements such as CU, PB, SN are slightly enriched, and ZN is slightly poor (Table 5-3).
The noteworthy is that the elements such as CU, PB, Zn, MO, W, SN in the two long granite are highly enriched, and their values are PB: 78.0 × 10-6, Zn: 104.0 × 10-6, W: 159.0 × 10-6, MO: (2.69 ～ 24.1) × 10-6, SN: (3.88 ~ 11.0) × 10-6 (Table 5-3), which is more than a dozen to a few normal rocks. Ten times, it shows that the relationship with multi -metal mineralization is closely related, and it may be a mineral rock.
Table 5-3 Early middle-generation granite rock-like mineral element content table
continuation table
6. Mine -making heat source. The late Yanshan in the study area is shallow -ultra -shallow and middle -acid sexual invasion of rocks is closely related to gold mines. Become a low -temperature hot liquid mine.
The Yanshan period Due to the dive of the Pacific sector and the thickening of the rock ring in mainland China, a rock ring stretched, reduced, and disassembled the conversion process. Part of the melting of the mantar-source magma forms a medium-rich and multi-metallic element (Table 5-2) (Table 5-2) (Yang Tiezheng, 2008), and the thermal liquid and mineral fluid hot liquid rich in ore elements rose to In the shallow openings of the crust, with the continuous addition of atmospheric precipitation, the mineral fluids are cooled quickly. Most gold elements are enriched, forming a low -temperature heating -type gold mines.
In summary, the southeast of Xiaoxing'an Ridge is the pimyen type CU-AU mineral belt of the Silicon Cab-AU mineral belt and the shallow temperature thermal liquid-type AU mine belt ( Shade Ming et al., 2003; Ge Wenchun et al., 2007), they constitute a unified, organic structure -magma -mineral series.

1 thought on “Granite contain mine exclusive attribute analysis”

Nina
December 29, 2022 at 7:40 pm

The research zone is located in the Yichun -Yanshou Non -Metal Mine and Iron Mine Mining Ambuers (Han Zhenxin et al., 2004), the most important lead, zinc, iron, tungsten, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, molybdenum, and molybdenum, Waiting for a multi -metal symbiotic convergence zone. The invasive rock is widely revealed in this area, and its relationship with minerals is more closely related to minerals. It is mainly tungsten, molybdenum, lead, zinc, and iron mineral (points).
1. Ancient Yuan and ancient granite
The ancient crystal base in the research area Xingdong Rock Group and the iron rock layer in the Dongfeng Mountain Rock Group were invaded by regional deterioration and granite sage hemp rocks -under the action of thermal fluid Once again, the East Wind Magnetic quartz -type iron ore is formed.
The ancient Yuan Granite Film Miscellaneous Rock (PT1GN) is compared with the granite hemp rocks of the Grandma Miscellaneous Rock in Xing'an -Jihei Zengshan Belt in Inner Mongolia (Chi Qinghua et al., 2007). PB, SN enrichment, ZN, CR, NI and other elements have decreased, and the MO content is similar (Table 5-2). The relationship between the ancient Yuan ancient granite tablets and the gold mineralization of the ancient Yuan Gang is closely related. The average AU content of the ancient granite tablets hemp rock was 0.05 × 10-6 (Han Zhenxin et al., 2004). It can be speculated that the ancient crystal base rock is one of the mineral rocks of rock gold and sand gold. Jinfeng's value has significantly reduced its gold content from the ancient base metamorphic rock → granite sliced hemp rock (granite), indicating that the gold with granite is migrated, and the hot liquid gold mine may be formed under the right conditions. Essence In this work, in the ancient Yuan and ancient granite tablets of the Songlin Forest Farm of Xinqing Forestry Bureau, three new rock gold mineralized body was found in the deterioration of the metamorphic layers of the Dongfeng Mountains. Therefore, pay attention to finding rock gold mines in the ancient crystal base.
2. The ancient granite of the Chinese and premium
is mainly ultra-magnesium-iron magnesium miscellaneous rocks, which are produced with rock-shaped output. In the rock group, the high -voltage blue rock phase with Heilongjiang Rocks -deep -pressure green sliced rock -like deep -sea silicon deposits, medium base sea rock rocks, etc., constitute the ancient Taipinggou -Golden Mine Forest Snake Green Rock Set ( Cao Yan et al., 1992; Qiqihar Branch, Heilongjiang Province, 2006). Miscellaneous rocks are composed of snake -grained rocks, penetrating glitter rocks, and green mud rock rocks. The content of trace elements CR, Ni, and CO of rocks is very high, and it is 2010 × 10-6 to 2600 × 10-6, 1340 × 10-6 ～ 1860 × 10-6, 59.7 × 10-6 ～ 83.8 × 10-6 (Table), its magma comes from the source of the mantle. They have a cause of contact with the minerals, which can be CR, Ni, and CO ore sources. Compared with the ultra-magnesium iron rock in the eastern part of China (Chi Qinghua et al., 2007), the content of CU, PB, Zn, AU, SB is reduced, the MO content is similar, and the rich SN element is characterized (Table 5-2).
Thetegly granite trace element content in different times of the research area of different times of the research area
If in the ancient Jiamusi plot in the stretch structure environment to form a small ocean basin During the collage, the magnesium iron quality -ultra -magnesium iron miscellaneous rock was broken in the reducing zone, and then the characteristics of linear beadin -like distribution were broken along the backbuilding or sliding break -off fault, which explained China -Yuan ancient snake green rocks (magnesium iron -ultra -magnesium iron miscellaneous rocks) constructed constructive invasion of collage collage collaboration collaboration -arc land collage and make them mutually collage hyperplasia, becoming the ancient and hyperplasia of China Part of the band.
3. Gali East Period granite
This granite is near SN to the band to the band of Yichun -Yanshou fold system and Xingkai Lake -Lao Lingling plot. That is, near the west side of the Mudanjiang Deep Fracture Belt. The granite ingredients have changed greatly in this period. From early to late rock types, the type of lithography has evolved from quartz glittering long rocks → granite flashes long rock → second -long granite. The type of rock type evolved from neutral → acidity. It is a relatively complete sequence of component evolution. In the wild macro, different ingredients of rocks are interspersed with each other, wrapped and gradient contact relationships. In advanced rock body, magma mixing the cause of magma mixed with the MME type microclican long -quality bag, which has a significant shell mixture mixed rock phase learning. , Rock Chemical, Earth Chemical characteristics. The rock body is formed in the edge environment of the continental curved activity of the land edge, which may represent the collapse of the collage between the collage between the combination and collage between the Jiamusi plot between the Jiamusi plot in the early ancient generation. The shell mantle mixed effect (Han Zhenzhe et al., 2009B) under the influence of the bottom invasion, which has broaden ideas for the research of Gali East Period granite in the region.
The trace elements in the second long granite of the Gali East phase comparison with the average value of the two long granite with the second long granite of the Xing'an -Jihei Crream Mountains in Inner Mongolia (Chi Qinghua et al., 2007), CU, PB, Zn, MO, W, SN and other elements are enriched. The content of AU and AG is low (Table 5-2), and elements such as CU, PB, Zn, MO, SN in Government Flashing and Flashing rocks are also rich. This issue is closely related to PB, Zn, W, MO, and Fe mineralization, which constitutes the first period of the first phase of Yichun -Yanshou Nonferrous Metal and Iron Mine Mine. The important heat source of contact type and thermal liquid minerals in China.
Ilin (super) large lead zinc mine and iron multi -metal mineral beds are related to typical mines related to Gali East period granite. Similar, and the PB isotope composition of the sedimentary rock sedimentation of the lead mountain group is relatively large, reflected in minerals mainly from magma (Han Zhenxin et al., 2004), indicating that the source of the magma may be rich in PB, Zn, etc. In the process, further extension with magnesium -rich carbonate surrounding rocks, drawing the mineral division in the surrounding rock, and with the differentiation of the magma, the mining group is continuously enriched in the magma, lead zinc zinc, and lead zinc zinc Minerization is a large amount of precipitation in accordance with the filling and explanation method, forming a low -temperature heat -charging -contact -type lead -zinc mine.
4. Huali West Period granite
This in the middle of Huali West in the middle of Huali West, anesthetic medium granules (ring spots) two long granite invading the Dali of the East Fengshan Rock in the ancient Yuan Dynasty, forming Silicon stroke -type groups of iron ore, Golden River zinc iron ore, field cannon lead zinc ore point, etc. The ore body is mainly produced in the internal and external contact zone, and a few are produced in the second -long granite of the eclipse. The weak sliced siber -like medium granules (ring spots) and the two -long granite invaded the lead mountain group of the Cambrian Xilin group under the Silicon Calcium Rock type Xiying Iron Mineralization Point. Dali rocks in the Ling Group form a large Kunlun iron ore filled with a Silicon Calcium type -thermal fluid. In summary, when Huali West invades rocks into the above -mentioned strata, the invasive contact belts are invaded and formed to form horny, silicon blocons, and mineralization such as iron, lead, and zinc. type. In the northern Dabao Mountain area of Xiaoxing'an Ling, Hualili West Period granite is closely related to CU, MO, AU, and FE, and has a strong mineral effect (Du Qi, 1988).
It -shaped siber -shaped medium grains like spots (ring spots) two long granite, granite flashes long rocks and other rocks with the average value of the two long granite in Inner Mongolia -Jihei Creation Mountain (Chi Qinghua et al., 2007), CU, CU, CU, CU, CU, CU, ZN, MO, W, SN and other elements are enriched. PB and AG have basically no change, while AU, NI and other elements are poor (Table 5-2), indicating that the rocks may be multi-metal CU, Zn, MO, W, Sn, etc. One of the mineral rocks of mineral elements. In addition, it is worth mentioning that the content of mineral elements such as CU, Zn, MO, etc. in the fine -grained long quality bag is significantly higher than that of the host rock (Han Zhenzhe et al., 2008A), implying that there are many iron, more iron, more iron and more in the southeast of Xiaoxing'an Ridge. Metal beds are closely related to the mixing effect of magma, which may be related to the ore elements such as CU, MO, PB, Zn, FE, and other mineral elements.
5. Indiacopy Period granite
This granite invasion in this issue is strong, which is one of the main heat sources of Xiaoxing'an Ridge -Zhangguangcai Laoling Metal Mining Belt One of the mineral rocks. The dewy is mainly based on the combination of spots -like two -long granite. This issue of granite is the key research object of this book. Its detailed rock science, main trace, isotope, and the characteristics of mineralization are shown in the third and fourth primary chapters.
The comparison with the average value of the two long granite in Inner Mongolia -Jihei Building Mountain with two long granite (Chi Qinghua et al., 2007), CU, Zn, MO, W, SN and other elements in the spots are rich. The PB content is close, and AG is slightly poor. Among them, the fine-grained giant spots-like two-long granite CU and W are the most enriched. The CU value is as high as 144.3 × 10-6, which is dozens of times higher. The granite is the highest, up to 2.6 × 10-6, more than several times high, and W is also the highest in the giant giant spots in the fine-grained giant spots. In the long-alkali-long granite, W and MOs are the most enriched. The elements such as CU, PB, SN are slightly enriched, and ZN is slightly poor (Table 5-3).
The noteworthy is that the elements such as CU, PB, Zn, MO, W, SN in the two long granite are highly enriched, and their values are PB: 78.0 × 10-6, Zn: 104.0 × 10-6, W: 159.0 × 10-6, MO: (2.69 ～ 24.1) × 10-6, SN: (3.88 ~ 11.0) × 10-6 (Table 5-3), which is more than a dozen to a few normal rocks. Ten times, it shows that the relationship with multi -metal mineralization is closely related, and it may be a mineral rock.
Table 5-3 Early middle-generation granite rock-like mineral element content table
continuation table
6. Mine -making heat source. The late Yanshan in the study area is shallow -ultra -shallow and middle -acid sexual invasion of rocks is closely related to gold mines. Become a low -temperature hot liquid mine.
The Yanshan period Due to the dive of the Pacific sector and the thickening of the rock ring in mainland China, a rock ring stretched, reduced, and disassembled the conversion process. Part of the melting of the mantar-source magma forms a medium-rich and multi-metallic element (Table 5-2) (Table 5-2) (Yang Tiezheng, 2008), and the thermal liquid and mineral fluid hot liquid rich in ore elements rose to In the shallow openings of the crust, with the continuous addition of atmospheric precipitation, the mineral fluids are cooled quickly. Most gold elements are enriched, forming a low -temperature heating -type gold mines.
In summary, the southeast of Xiaoxing'an Ridge is the pimyen type CU-AU mineral belt of the Silicon Cab-AU mineral belt and the shallow temperature thermal liquid-type AU mine belt ( Shade Ming et al., 2003; Ge Wenchun et al., 2007), they constitute a unified, organic structure -magma -mineral series.

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