2023
General information and occurrence
This group of mineral raw materials mainly comprises metals, which are the accompanying elements in sulfides ores. Such elements occur mainly in zinc-lead ores deposits within the Silesian-Cracow region and copper-silver ores deposits in the Fore-Sudetic Monocline and in the North Sudetic Basin. The elements are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in the evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements (REE) and those named as dispersed elements were also found in beach sands of: the Ławica Słupska deposit (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and the Ławica Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.13 million m3 of brines in the Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Resources and output
The total resources volume of the elements coexisting in ores and other raw materials are shown in Table 1.
The state of resources exploration and the state of their development together with the magnitude of depletion in resources of elements co-occurring in lead and zinc deposits and copper and silver deposits are presented in Table 2 and Table 3, respectively. The part of estimated resources of these elements co-occurring in Cu-Ag ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Agnieszka Malon, Marcin Tymiński, Stanisław Z. Mikulski
2022
General information and occurrence
This group of mineral raw materials mainly comprises metals, which are the accompanying elements in sulfides ores. Such elements occur mainly in zinc-lead ores deposits within the Silesian-Cracow region and copper-silver ores deposits in the Fore-Sudetic Monocline and in the North Sudetic Basin. The elements are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in the evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements (REE) and those named as dispersed elements were also found in beach sands of: the Ławica Słupska deposit (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and the Ławica Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.14 million m3 of brines in the Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Resources and output
The total resources volume of the elements coexisting in ores and other raw materials are shown in Table 1.
The state of resources exploration and the state of their development together with the magnitude of depletion in resources of elements co-occurring in lead and zinc deposits and copper and silver deposits are presented in Table 2 and Table 3, respectively. The part of estimated resources of these elements co-occurring in Cu-Ag ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Agnieszka Malon, Marcin Tymiński, Stanisław Z. Mikulski
2021
General information and occurrence
This group of mineral raw materials mainly comprises metals, which are the co-occurring elements in sulfides ores. Such elements occur mainly in zinc-lead ores deposits and copper-silver ores deposits in the Fore-Sudetic Monocline and in the North Sudetic Basin. The elements are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in the evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: the Ławica Słupska deposit (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and the Ławica Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase)), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.14 million m3 of brines in the Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Resources and output
The total resources volume of the elements coexisting in ores and other raw materials are shown in Table 1.
The state of resources exploration and the state of their development together with the magnitude of depletion in resources of elements co-occurring in lead and zinc deposits and copper and silver deposits are presented in Table 2 and Table 3, respectively. The part of estimated resources of these elements co-occurring in Cu-Ag ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Agnieszka Malon, Marcin Tymiński, Stanisław Z. Mikulski
2020
General information and occurrence
This group of mineral raw materials mainly comprises metals, which are the co-occurring elements mainly in sulfides ore deposits. Such elements occur mainly in zinc-lead ores deposits and copper ores deposits and are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in the evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and Ławica Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase)), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.14 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Resources and output
The total resources volume of the elements coexisting in ores and other raw materials are shown in Table 1.
The state of resources exploration and the state of their development together with the output magnitude of elements co-occurring in lead and zinc deposits and copper deposits are presented in Table 2 and Table 3, respectively. The part of indicated/inferred (estimated) resources of these elements co-occurring in copper ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Stanisław Z. Mikulski
2019
General information and occurrence
This group of mineral raw materials mainly comprises metals, which are the co-occurring elements mainly in sulfides ore deposits. Such elements occur mainly in zinc-lead ores deposits and copper ores deposits and are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in the evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and Ławica-Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase)), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.14 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Resources and output
The total resources volume of the elements coexisting in ores and other raw materials are shown in Table 1.
The state of resources exploration and the state of their development together with the output magnitude of elements co-occurring in lead and zinc deposits and copper deposits are presented in Table 2 and Table 3, respectively. The part of indicated/inferred (estimated) resources of these elements co-occurring in copper ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Stanisław Z. Mikulski
2018
This group of mineral raw materials mainly comprises metals, which are co-occurring elements mainly in sulfides ore deposits. Such elements occur mainly in zinc-lead ores deposits and copper ores deposits and are being already recovered or may be recovered in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and Ławica-Odrzana deposit (geological resources approved in 2014 are equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3 (ilmenite), 20.23 thousand tonnes of TiO2 (rutile, anatase)), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in brines (32.14 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations have not been made since then.
Table 1 shows a summary of resources estimations of major co-occurring elements (thousand tonnes).
The state of resources exploration and the state of their development together with the output magnitude of elements co-occurring in lead and zinc deposits and copper deposits are presented in Table 2 and Table 3, respectively. The part of indicated/inferred (estimated) resources of these elements co-occurring in copper ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Stanisław Z. Mikulski
2017
This group of mineral raw materials mainly comprises metals, which are co-occurring elements mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of a high market value, are already recovered or may become recoverable in the course of the processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted usually in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources equal: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes of TiO2) and Ławica-Odrzana deposit (geological resources approved in 2014 equal: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3, 20.23 thousand tonnes of TiO2), in potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and in saline waters and brines (32.16 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for the Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations has not been made since then.
Table 1 shows a summary of resources estimations of major co-occurring elements (thousand tonnes).
The state of resources exploration and the state of their development together with the output magnitude of elements co-occurring in lead and zinc deposits and copper deposits are presented in Table 2 and Table 3, respectively. The part of indicated/inferred resources of these elements co-occurring in copper ores deposits has been determined within anticipated sub-economic resources of the ore.
Prepared by: Stanisław Z. Mikulski
2016
This group of mineral raw materials mainly comprises metals, which are co-occurring elements mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of a high market value, are already recovered or may become recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by the prospecting and exploration which resulted often in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes TiO2) and Ławica-Odrzana deposit (geological resources approved in 2014: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3, 20.23 thousand tonnes of TiO2), potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and saline waters and brines (32.16 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations has not been made since then.
Table 1 shows a summary of estimations of resources of major co-occurring elements (thousand tonnes).
Prepared by: Stanisław Z. Mikulski
2015
This group of mineral raw materials mainly comprises metals, which are co-occurring elements mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of high market value, are already recovered or may become recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by prospecting and exploration which resulted often in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands of: Ławica Słupska (estimated resources: zirconium – 2 thousand tonnes of ZrSiO4; titanium – 12 thousand tonnes TiO2) and Ławica-Odrzana deposit (geological resources approved in 2014: zirconium – 25.28 thousand tonnes of ZrSiO4, titanium – 156.78 thousand tonnes of FeTiO3, 20.23 thousand tonnes of TiO2), potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and saline waters and brines (32.16 million m3 of brines in Łapczyca deposit). The data on boron, bromine, zirconium and titanium (except for Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations has not been made since then.
Table 1 shows a summary of estimations of resources of major co-occurring elements (thousand tonnes).
In 2015 there was a new copper ores deposit – Radwanice-Gaworzyce – documented and the resources of co-occurring elements were assessed. The calculations were made for: lead, cobalt, molibdenium, nickel and vanadium (table 3).
Prepared by: Stanisław Z. Mikulski
2014
This group of mineral raw materials mainly comprises metals, which occur as co-occurring elements mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of high market value, are already recovered or may be recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by prospecting and exploration which resulted often in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands (zirconium – 2 thousand tonnes; titanium – 12 thousand tonnes), sands of Ławica-Odrzana deposit (zirconium – 25.28 thousand tonnes, resources documented in 2014), potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and saline waters and brines (32.16 million m3). The data on boron, bromine, zirconium and titanium (except for Ławica Odrzana area) come from the evaluations made in 1960s and any new calculations has not been made since then.
Table 1 shows a summary of estimations of resources of major co-occurring elements (thousand tonnes).
In 2014 there was new zinc and lead ores deposit – Zawiercie 3 – documented and the resources of co-occurring elements were assessed. The calculations were made for: arsenic, gallium, germanium, cadmium, sulphur, silver and thallium (table 2).
Prepared by: Stanisław Z. Mikulski
2013
This group of mineral raw materials mainly comprises metals, which occur as co-occurring elements mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of high market value, are already recovered or may be recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by prospecting and exploration which resulted often in evaluations of their indicated/inferred resources. Sometimes their resources are documented.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands (zirkonium – 2 thousand tonnes; titanium – 12 thousand tonnes), potassium-magnesium salts (boron – 6 thousand tonnes; bromine – 7.2 thousand tonnes) and saline waters and brines (32.16 million m3). These numbers were evaluated in 1960s and there have not been any new calculations prepared so far.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands and saline waters and brines.
ZGH “Bolesław” S.A. company informed that due to longlasting exploitation of zinc and lead ores deposits – Olkusz and Pomorzany – the resources of co-occurring elements (cadmium, sulfur and silver) decreased significantly.
Prepared by: Stanisław Z. Mikulski
2012
This group of mineral raw materials mainly comprises metals which deposits have not been hitherto discovered in Poland and the domestic demand is fully covered by import, except for some amounts which are or may be recovered from processing and recycling non-mineral waste-derived raw materials. Metals assigned to this group include aluminum, chromium, magnesium and manganese as well as several elements of smaller economic importance such as antimony, cobalt and noble metals.
Metallic elements occur mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of high market value, are already recovered or may be recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by prospecting and exploration which resulted often in evaluations of their indicated/inferred and sometimes even geological resources. Further fate of resources of these metals will depend on domestic demand and changes in prices at the international markets.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands and saline waters and brines.
The changes in estimated resources are the result of new documentations accepted for several copper deposits – Lubin-Małomice, Polkowice, Rudna and Sieroszowice.
Prepared by: Stanisław Z. Mikulski
2011
This group of mineral raw materials mainly comprises metals which deposits have not been hitherto discovered in Poland and the domestic demand is fully covered by import, except for some amounts which are or may be recovered from processing and recycling non-mineral waste-derived raw materials. Metals assigned to this group include aluminum, chromium, magnesium and manganese as well as several elements of smaller economic importance such as antimony, cobalt and noble metals.
Metallic elements occur mainly in sulfides ore deposits. This is the case of Polish copper and zinc-lead deposits with fairly long records of various co-occurring elements. The elements, often of high market value, are already recovered or may be recoverable in the course of processing of these ores. Accumulations of some of these elements were covered by prospecting and exploration which resulted often in evaluations of their indicated/inferred and sometimes even geological resources. Further fate of resources of these metals will depend on domestic demand and changes in prices at the international markets.
Rare earth elements and those named as dispersed elements were also found to occur in beach sands and saline waters and brines.
Prepared by: Stanisław Z. Mikulski