Beijing Donia Resources Co.

Beijing, China

Beijing Donia Resources Co.

Beijing, China
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Wang L.-Q.,Chinese Academy of Geological Sciences | Gu X.-X.,China University of Geosciences | Tang J.-X.,Chinese Academy of Geological Sciences | Wang H.,Chinese Academy of Geological Sciences | And 3 more authors.
Journal of Chengdu University of Technology (Science and Technology Edition) | Year: 2011

The paper studies the source and characteristics of the ore-forming fluids in the Mengya'a Pb-Zn deposit of Tibet and identifies the genetic type of deposit by studying the typical deposit of this area. It analyzes the altered limestone in the surrounding area, the carbon and oxygen isotopes of hydrothermal calcite and the hydrogen and oxygen isotopes of quartz formed in different mineralization periods, studies the fluid inclusions petrographically, and measures their temperatures and salinity. The resuct shows that in the early post-mineralization stage, the ore-forming fluids were was mainly in the form of magmatic water, while in the later stage, they were mixed with plentiful meteoric water. In the mineralization period, ore-forming fluids were generally characterized by medium-high temperatures and intermediate-low salinity and there was an apparent temperature-dropping trend from the early to the late ore-forming stage. The formation of the deposit is closely related to magmatism and the deposit is a zinc-lead one under the skarn type.

Han S.,University of South China | Han S.,Central South University | Zhang S.,Central South University | Liu J.,Central South University | And 3 more authors.
Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences | Year: 2014

There are pre-, syn-, and post-orogenic granites in Shire region of northern Ethiopia. Whole rock Sm-Nd isochron dating results show that diagenetic age of pre-, and post-orogenic ages are 824.4±15.5 Ma and 517.9±5.8 Ma respectively. Major, rare-earth and trace elements of three kinds of granite are obviously different. The pre-orogenic granites are relatively low in MgO and high in SiO2, belonging to the peraluminous series granite, with low K content and slight light REE enrichment, high large-ion lithophile element abundance and relative depletion of HFSE.The syn-orogenic granite belongs to the quasi-aluminous rock and high-potassium calc-alkaline granite, with the light REE enriched pattern, high large-ion lithophile element and HFSE abundances. The post-orogenic granite belongs to the weakly peraluminous high-potassium calc-alkaline granite, which has the chondrite-normalized REE patterns in the type of "gull" with severe depletion in Eu. The large-ion lithophile elements are concentrated, while P and Ti are severely depleted here. Comprehensive study shows both the pre- and syn-orogenic granites are I-type mantle-source granites in the passive continental margin-volcanic island arc tectonic setting; the post-orogenic granites are A2-type crust-source major granites, which were formed from the melting of thinner crust after the closure of oceanic basins and the growth of Arabian-Nubian shield.

Jia R.-X.,Chinese Academy of science | Jia R.-X.,Beijing Exploration Technology Center for Mineral Resources | Jia R.-X.,Beijing Donia Resources Co. | Fang W.-X.,Chinese Academy of science | And 2 more authors.
Kuangwu Yanshi/ Journal of Mineralogy and Petrology | Year: 2011

The NM deposit is located in the northwest trending magmatic-tectonic belt, northcentral part of Truong Son, which was subjected to right-lateral shearing due to the collision of Sibumasu micro-continent with Indo-China micro-continent along Nan-Uttaradit suture during Permian-Triassic Period. Based on the grain size and spatial distribution,the granites in NM deposit can be classified into medium-coarse grained granite, porphyritic granite and fine grained granite respectively. The geochemical characteristics of different types of granite show that they are high-potassium, calc-alkaline granitoids with the ACNK ratios mostly ranging from 0.9 to 1. 1. Trace elements of the granites show that the variety of LILE enriches in Cs, Rb, Th, U,K, while depletes in Ba and Sr,distinct fractionation of HFSE with clearly negative anomaly of Nb,P and Ti. REE analysis reveals relative high content and distinct fractionation of LREE in contrast to HREE,and moderate to sharp negative Eu anomaly. All of the geochemical features indicate that these different types of granites in NM deposit were derived from the same origin related to the special tectonic setting of post-collision volcanic arc. During the magmatic evolution process from early stage represented by medium-coarse grained granite to last stage represented by fine grained granite, the TFe, TiO 2, MgO 1CaO and Na 2O contents in magma tend to decrease, while the SiO 2 and K 2O contents increase gradually, and the Fe,Cu and Zn (Pb) mineralization is mainly related to the porphyritic granite.

Han S.-L.,Central South University | Zhang S.-G.,Central South University | Liu J.-X.,Central South University | Hu H.-J.,Central South University | And 2 more authors.
Transactions of Nonferrous Metals Society of China (English Edition) | Year: 2013

In mineral exploration, the apparent resistivity and apparent frequency (or apparent polarizability) parameters of induced polarization method are commonly utilized to describe the induced polarization anomaly. When the target geology structure is significantly complicated, these parameters would fail to reflect the nature of the anomaly source, and wrong conclusions may be obtained. A wavelet approach and a metal factor method were used to comprehensively interpret the induced polarization anomaly of complex geologic bodies in the Adi Bladia mine. Db5 wavelet basis was used to conduct two-scale decomposition and reconstruction, which effectively suppress the noise interference of greenschist facies regional metamorphism and magma intrusion, making energy concentrated and boundary problem unobservable. On the basis of that, the ore-induced anomaly was effectively extracted by the metal factor method. © 2013 The Nonferrous Metals Society of China.

Han S.-L.,Central South University | Zhang S.-G.,Central South University | Liu J.-X.,Central South University | Ding J.,Central South University | And 3 more authors.
Zhongnan Daxue Xuebao (Ziran Kexue Ban)/Journal of Central South University (Science and Technology) | Year: 2012

Taking the meta-volcanics in Shire region of Ethiopia northern as a typical instance, the lithology lithofacies characteristics of the meta-volcanics cycle were compound, and the technology and method were discussed to identify volcanic cycle and rhythm by using geochemical data. Through the geological and geochemical section analysis, this method selects the representative geochemical elements Si and Fe+Mg content as analysis object and db5 wavelet bases for the three-scale after wavelet decomposition and reconstruction. Synthetically comparing the spatial distribution characteristics of the geological section, the meta-volcanics were divided into 6 cycles and 15 rhythm. The results show that wavelet processing, the geochemical data effectively remove the local noise interference and extract the information about cycle and rhythm. The wavelet analysis plays a unique function and effect in discrimination of volcano cycle, i.e. it not only effectively divides the regional volcanic cycle, but also validly identifies the rhythm inside volcanic cycle.

Jia R.,Chinese Academy of science | Jia R.,Beijing Exploration Technology Center for Mineral Resources | Jia R.,Beijing Donia Resources Co. | Fang W.,Chinese Academy of science | And 2 more authors.
Journal of Rare Earths | Year: 2010

The NM copper polymetal deposit is located in the middle north part of the Truong Son metallogenic belt in Laos, which is the skarn-typed deposit and located in the contact between Indosinian granite and Lower Carboniferous limestone. All the ore-bodies in NM deposit can be divided into four types according to their occurrences: I copper ore-body as the massive restite developed in inner contact near the granite in north part; II-1 zinc-copper ore body and II-2 copper-iron ore body developed within contact between the granite and carbonate rocks, III copper-zinc ore body developed in the cranny among the southern carbonate stratum, indicating that all the ore-bodies were related to Indosinian granite emplacing into the Carboniferous limestone and causing the metallogenic system from closed state getting into half open state. The geochemical characteristics and mineral assemblages of them showed that all the orebodies in NM deposit derived from a similar origin and their ore-forming fluids with the evolution trend from reductive state in early stage to oxidative state in later stage were mainly related to the coupling interaction between post-magmatic hydrothermal fluid and basin fluid. Copyright © 2012 Elsevier B.V.

News Article | November 3, 2016

VANCOUVER, BRITISH COLUMBIA--(Marketwired - Nov. 3, 2016) - Nickel North Exploration Corp. (TSX VENTURE:NNX) (the "Company" or "Nickel North") announces that, the Company entered into a loan agreement (the "Loan Agreement") with SinoTech (Hong Kong) Corporation Limited (the "Lender"), pursuant to which the Lender agreed to make a loan in the amount of $300,000 to the Company by November 15, 2016. The principal sum of the loan under the Loan Agreement bears interest at a fixed rate of 8% per annum and the maturity date of the loan is December 31, 2016. The Lender is a wholly-owned subsidiary of Sinotech Minerals Exploration Co., Ltd. ("Sinotech Minerals Exploration"). Sinotech Minerals Exploration is a majority owner of Beijing Donia Resources Co., Ltd., which wholly-owns Goldrock Resources Corporation Limited ("Goldrock"). Goldrock and the Lender, together, own 48,071,860 common shares of the Company, (21,271,860 common shares for Goldrock and 26,800,000 common shares for the Lender), representing approximately 62.8% of the issued and outstanding common shares of the Company. The proceeds of the loan are expected to be used by the Company for the daily operation and paying the current liabilities. As a material change report in connection with the Loan Agreement is being filed less than 21 days before the closing of the Loan Agreement, there is a requirement under Multilateral Instrument 61-101 Protection of Minority Security Holders in Special Transactions to explain why the shorter period was reasonable or necessary in the circumstances. In the view of the Company, such shorter period was reasonable and necessary in the circumstances to improve the Company's financial position such that the Company can pay for the daily operation and the current liabilities. Nickel North Exploration is a Canadian based explorer focused on defining a Ni-Cu-PGE resource at our Hawk Ridge Project in Northern Quebec. The board of directors, advisor committee and management team are experienced, successful mine finders. The property consists of a 50 km long belt of magmatic Ni-Cu-PGE occurrences covering over 30,658 hectares. The project is located near tidewater. Quebec is a mining friendly jurisdiction. Nickel North Exploration is a conscientious corporate citizen, maintains good relations with Communities and Aboriginal people, and is committed to sustainable development. For more information on the company, please visit Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release. All statements, other than statements of historical fact, included herein are forward-looking statements that are subject to risks and uncertainties. Forward-looking statements are often, but not always, identified by the use of words such as "seek", "anticipate", "believe", "plan", "estimate", "expect", "likely" and "intend" and statements that an event or result "may", "will", "should", "could" or "might" occur or be achieved and other similar expressions. Forward-looking statements in this news release include a statement that the proceeds of the loan are expected to be used by the Company for the daily operation and paying the current liabilities. Forward-looking statements are subject to business and economic risks and uncertainties and other factors that could cause actual results of operations to differ materially from those contained in the forward-looking statements. Important factors that could cause actual results to differ materially from the Company's expectations include fluctuations in commodity prices and currency exchange rates; uncertainties relating to interpretation of drill results and the geology, continuity and grade of mineral deposits; the need for cooperation of government agencies and native groups in the exploration and development of properties and the issuance of required permits; the need to obtain additional financing to develop properties and uncertainty as to the availability and terms of future financing; the possibility of delay in exploration or development programs and uncertainty of meeting anticipated program milestones; and uncertainty as to timely availability of permits and other governmental approvals. Forward-looking statements are based on estimates and opinions of management at the date the statements are made. The Company does not undertake any obligation to update forward-looking statements except as required by applicable securities laws. Investors should not place undue reliance on forward-looking statements.

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