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Energy and tellurium deposits

  • Received: 05 November 2023 Revised: 20 December 2023 Accepted: 11 January 2024 Published: 19 January 2024
  • In this article, we focus on the next generation of green batteries that are closely related to semi-metallic tellurium and its deposits. We briefly summarize the chemical and geochemical characteristics of tellurium that ordinary readers are not familiar with or have never heard of, and its important role in many fields such as high-tech and medical care, current global resource distribution, major mineral extraction and purification technologies and market evolution, etc. The spatiotemporal distribution of the two main types of tellurium deposits, namely associated tellurium deposits and independent tellurium deposits, is introduced in detail. The geological and geochemical characteristics of the only independent tellurium deposit in the world are introduced in detail, so that relevant researchers can use this deposit as an example to discover more independent tellurium deposits around the world, meeting people's increasingly urgent demand for tellurium and realizing the sustainable development of human society. We believe that humans will discover more and more new energy metals in the near future to meet the dual goals of protecting the earth's environment and developing the economy, which are contradictory and mutually reinforcing. New generation of energy metal batteries must be small, compact, easy to carry, charge quickly, and have a long life.

    Citation: Jianzhao Yin, Haoyu Yin, Yuhong Chao, Hongyun Shi. Energy and tellurium deposits[J]. AIMS Geosciences, 2024, 10(1): 28-42. doi: 10.3934/geosci.2024002

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  • In this article, we focus on the next generation of green batteries that are closely related to semi-metallic tellurium and its deposits. We briefly summarize the chemical and geochemical characteristics of tellurium that ordinary readers are not familiar with or have never heard of, and its important role in many fields such as high-tech and medical care, current global resource distribution, major mineral extraction and purification technologies and market evolution, etc. The spatiotemporal distribution of the two main types of tellurium deposits, namely associated tellurium deposits and independent tellurium deposits, is introduced in detail. The geological and geochemical characteristics of the only independent tellurium deposit in the world are introduced in detail, so that relevant researchers can use this deposit as an example to discover more independent tellurium deposits around the world, meeting people's increasingly urgent demand for tellurium and realizing the sustainable development of human society. We believe that humans will discover more and more new energy metals in the near future to meet the dual goals of protecting the earth's environment and developing the economy, which are contradictory and mutually reinforcing. New generation of energy metal batteries must be small, compact, easy to carry, charge quickly, and have a long life.



    Credit rating migration risk is an important kind of credit risk, referring to the possibility of potential losses due to changes in credit rating. The phenomenon of rating movements has long attracted the attention of academia and industry and there have been many studies on the performance and patterns of credit rating transitions [1,2,3,4,5,6]. As for the valuation of credit migration risk, the used models are mainly categorized into two types: the reduced-form model and the structural model. The former employs a transition density matrix to characterize the process of credit rating migrations, such as [7,8,9] while the latter utilizes the company's own financial status as the determinant of credit rating changes, such as [10,11,12,13]. Each kind of model has its advantages, but the structural model elucidates the mechanism of credit migration by explicitly linking credit ratings to the company's assets and liabilities.

    Liang and Zeng ([10], 2015) constructed the first structural model for assessing credit migration risk by pricing a corporate bond with this risk. By predefining an asset threshold as the boundary for credit migration, the company's asset values are divided into high and low rating regions. In different regions, the asset values follow geometric Brownian motions with different volatilities. The model was derived as an initial value problem of parabolic differential equations which are coupled on a fixed inner boundary. Further, Hu et al. ([11], 2015) took the asset-liability ratio as a threshold for credit migration and deduced the migration boundary as a free boundary. On these bases, more theoretical analyses are provided, such as the asymptotic traveling wave solution [14], convergence rate of the difference scheme [15], multi-credit rating case [16], steady-state solution [17], etc (see also [18,19,20,21,22]). There are also some empirical results for the single threshold model, for instance, the credit migration boundary was identified by pricing long-term bonds in the U.S. corporate bond market [23]. In those models with the fixed boundaries or free boundaries, the thresholds for upgrades and downgrades are the same. However, this single threshold may lead to infinite frequent changes in credit ratings within a short period, due to the assumption that asset values follow Brownian motions which can cross any level infinitely many times within any time interval. Chen and Liang ([12], 2021) made an improvement based on the free boundary model by introducing different asset-liability ratio thresholds for upgrades and downgrades, resulting in a pair of migration boundaries. As a buffer zone is formed between these two boundaries, the frequency of credit rating migrations per unit time becomes finite. Liang and Lin ([13], 2023) made a similar modification, applying a pair of asymmetric asset thresholds to the fixed boundary model, and obtaining a system of partial differential equations coupled with each other on a pair of fixed boundaries. Liang and Lin ([24], 2023) further explored an asymptotic traveling wave solution with a buffer zone for this kind of model.

    These structural credit migration models with thresholds are somewhat similar in form to the credit barrier model considered in Albanese and Chen ([3], 2006). A stochastic process with state-dependent volatilities was used to model the credit quality process, which directly indicated the dynamic of credit rating, with barrier crossings corresponding to credit migrations and default events, in Albanese and Chen ([3], 2006). The variable of credit quality might capture the firm's fundamental information but did not articulate specific implications in finance. In the structural models of Liang et al., the credit migrations were delineated by the crossings of the thresholds as well, with the driving factors explicitly identified as the asset value or the asset-liability ratio. Since the asset value was assumed to follow the Brownian motion with different volatilities in different ratings, the distribution of future asset value depends on only the current rating and value of asset, and not on the history of previous states, even in the structural models with buffer zones. Therefore, these models we analyze in this paper cannot capture non-Markov effects in rating transition probabilities, such as those identified in Lando and Skødeberg ([4], 2002), Nickell et al. ([6], 2000), etc.

    According to whether or not the upgrade threshold and downgrade threshold are the same, the structural models are classified into the single threshold model and the model with different upgrade and downgrade thresholds. We already know that substituting a pair of asymmetric thresholds for a single threshold avoids high-frequency fluctuations in credit ratings. However a natural question arises: What is the relationship between those two kinds of models? Intuitively, when upgrade threshold and downgrade threshold are very close, the asymmetric threshold model's behavior should be similar to that of a single threshold model. This article attempts to answer this question rigorously within the scope of the credit migration problem with fixed boundaries. We consider two fixed boundary models: one model from [10] with X(X>0) as a critical threshold for credit migration, and the other model from [13] with X as a threshold for downgrades, and Xε:=X+ε (depending on a small parameter ε>0) as a threshold for upgrades. By techniques of partial differential equations, we prove that the solution of the asymmetric threshold problem converges to that of the single threshold problem when the upgrade threshold Xε approaches the downgrade threshold X as ε0. To our knowledge, it is the first time that the asymptotic relationship between the single threshold and a pair of asymmetric thresholds has been shown in credit migration problems. Therefore, when ε is small enough, the different upgrade and downgrade threshold model can be approximated by a single threshold model, which already has more theoretical and empirical results.

    The remainder of the paper is organized as follows. In Section 2, the single threshold and the different downgrade and upgrade threshold model for credit migration problems with fixed boundaries are reviewed. In Section 3, we prove a series of lemmas to establish ε-independent estimates for the solution of the asymmetric threshold problem. In Section 4, a key step is shown that the first-order derivatives of the asymmetric threshold problem's solution on both sides of x=X tend to be equal, as ε approaches zero. It follows that the solution of this model converges to that of a single threshold model by compactness. Section 5 is a summary of this paper.

    The structural models with fixed migration boundaries assess credit rating migration risk by pricing a zero-coupon corporate bond.

    Let (Ω,F,P) be a complete probability space. Assuming that the company only issues one bond with a face value of 1 and a maturity of T, the bond is considered as a contingent claim of the company's asset value on the space (Ω,F,P). At maturity, the bond will default and pay out the remaining assets if the company's asset value is less than the face value of the bond. Let St denote the company's asset value in the risk-neutral world. It satisfies

    dSt={rStdt+σHStdWt, in high rating region, rStdt+σLStdWt, in low rating region, 

    where r is the risk-free interest rate, and

    σH<σL (2.1)

    represent volatilities (positive constants) of the company under the high and low credit grades respectively. Wt is the standard Brownian motion which generates the filtration {Ft}. High and low rating regions are determined by the company's asset value. Inequality (2.1) captures the characteristics of the high and low credit ratings, with the volatility of asset return in the lower rating region being greater than the volatility in the higher rating region.

    Liang and Zeng ([10], 2015) (referred to as LZ's model hereafter) gave a single predetermined threshold to divide asset value into high and low rating regions. Through a standard variable transformation x=logS and renaming Tt as t, we set the migration boundary as X(X>0) and represented the values of low and high-rated bonds as vL(x,t) and vH(x,t), respectively. The model is derived as the following partial differential equation problem:

    {vHt12σ2H2vHx2(r12σ2H)vHx+rvH=0,for x>X,t>0,vLt12σ2L2vLx2(r12σ2L)vLx+rvL=0,for x<X,t>0,vH(x,0)=min{ex,1},for x>X,vL(x,0)=min{ex,1},for x<X,vH(X,t)=vL(X,t),for t>0,vHx(X,t)=vLx(X,t),for t>0. (2.2)

    We define a solution v over the entire region (,)×[0,) as follows:

    v={vH(x,t), forxX,t0,vL(x,t), forx<X,t0. (2.3)

    Liang and Lin ([13], 2023) (referred to as LL's model hereafter) proposed a pair of asymmetric thresholds for credit migrations: one threshold for downgrades and the other slightly higher threshold for upgrades. After the same change of variables as in Section 2.1, we have set the downgrade threshold as X(X>0) and the upgrade threshold as Xε:=X+ε,ε>0. Denote by uLε(x,t) and uHε(x,t) the bond values in low rating and high rating, respectively. They are captured by the following PDE problem:

    {uHεt12σ2H2uHεx2(r12σ2H)uHεx+ruHε=0,for x>X,t>0,uLεt12σ2L2uLεx2(r12σ2L)uLεx+ruLε=0,for x<Xε,t>0,uHε(x,0)=min{ex,1},for x>X,uLε(x,0)=min{ex,1},for x<Xε,uHε(X,t)=uLε(X,t),for t>0,uLε(Xε,t)=uHε(Xε,t),for t>0. (2.4)

    Note that vLε and vHε overlap in [X,Xε]×[0,). To be comparable with v, we rearrange uε over the entire region as the following formula:

    uε={uHε(x,t), forxX,t0,uLε(x,t), forx<X,t0. (2.5)

    Letting the upgrade threshold Xε approach the downgrade threshold X, we find an asymptotic behavior of LL's model, i.e., as ε0, uε converges to v. This actuallly constructs an asymptotic relationship between LL's model and LZ's model. To prove this, we first establish some ε-independent estimates for the solution (uLε,uHε). Based on this, |uLεx(X,t)uHεx(X+,t)| approaching 0 as ε0 is verified as a key step. Further, we suggest that any convergent subsequence of uε tends to the solution v of LZ's model as ε0.

    Define Li=t12σi22x2(r12σi2)x+r,i=H,L; QLε=(,Xε)×(0,), and QH=(X,)×(0,).

    For any given ε, we iteratively define a sequence {uLεk,uHεk}k=0, which is proved to decrease with k and converge to (uLε,uHε) as k0 in Liang and Lin ([13], 2023). In detail, the sequence satisfies equations

    LL[uLεk]=0 in QLε, LH[uHεk]=0 in QH,

    with the initial value min{ex,1}. Starting from uLε0(Xε,t)1 and by the induction assumption uHεk(X,t)=uLεk(X,t) and uLε(k+1)(Xε,t)=uHεk(Xε,t), we have completed the definition of the sequence.

    The estimations of the maximum norm of (uLε,uHε) and its first-order derivative with respect to time t are carried out by induction on the sequence {uLεk,uHεk}k=0. As for the boundary estimate of (uLεx,uHεx), we introduce barrier functions.

    Lemma 3.1.

    0uLεmin{ex,1} in QLε, 0uHεmin{ex,1} in QH. (3.1)

    Proof. By the induction and maximum principle, for each k0, 0uHεkmin{ex,1} in QH, and 0uLεkmin{ex,1} in QLε.

    Lemma 3.2.

    C1uLεt0 in QLε¯Qρ, C1uHεt0 in QH, (3.2)

    where Qρ=(ρ/2,ρ/2)×(0,ρ2/4) and 0<ρ<X.

    Proof. We claim that C1uLεkt,uHεkt0 for any kN and C1 is independent of ε and k.

    Differentiating uLεk and uHεk with respect to t, they satisfy

    LL[uLεkt]=0 in QLε, LH[uLεkt]=0 in QH.

    On the migration boundaries, uLεkt(Xε,t)=uHε(k1)t(Xε,t) and uHεkt(X,t)=uLεkt(X,t).

    It is also clear that initially

    uLεkt(x,0)=0 forx<0,uLεkt(x,0)=r for0<x<Xε, (3.3)
    uHεkt(x,0)=r forx>X. (3.4)

    At x=0,uLεkxx(x,0) produces a Dirac measure of density 1. Thus, in the distribution sense,

    uLεkt(x,0)0 forx<Xε. (3.5)

    From the standard parabolic estimates (see e.g. [25]), there exists constants c1,c2 independent of ε and k, such that

    uLεktc2c2texp(c1x2t) for|x|<ρ2,0<tρ24,

    where 0<ρ<X. Take C1r such that

    C1c2+c2texp(c1x2t) on {|x|=ρ2,0<tρ24}{|x|<ρ2,t=ρ24}.

    It follows that on {xρ2,t=0}{|x|=ρ2,0<tρ24}{|x|<ρ2,t=ρ24}{ρ2xX,t=0},

    uLεktC1. (3.6)

    When k=0, uε0(Xε,t)=1 and we have uε0t(Xε,t)=0 on x=Xε for t>0.

    By further approximating the initial data with smooth functions if necessary, we conclude by (3.5) and maximum principle that

    uLε0t0 in QLε.

    We conclude by (3.6) and minimum principle that

    uLε0tC1 in QLε¯Qρ,

    where Qρ=(ρ/2,ρ/2)×(0,ρ2/4).

    We assume that C1uLεkt0 in QLε¯Qρ holds for k1. Since uHεkt(X,t)=uLεkt(X,t) for t>0 and (3.4), we conclude by extremum principle

    C1uHεkt0 in QH.

    From uLε(k+1)t(Xε,t)=uHεkt(Xε,t) and (3.5), (3.6), applying the extremum principle gives

    C1uLε(k+1)t0 in QLε¯Qρ.

    Thus, by induction, we derive that C1uLεkt0 in QLε¯Qρ and C1uHεkt0 in QH for any k0 and C1 is independent of ε and k. The lemma's results can be obtained by taking limits with k.

    Lemma 3.3.

    |uLεx|C2 in QLε, |uHεx|C3 in QH. (3.7)

    Proof. We estimate uLεx as an example and the same process works for uHεx.

    We fixed ε and first deal with the uLεx(Xε,t). Let K1(ρ<K1<X) be a constant and η=XK1. Define wLε=uLεXεxXεK1uLε(K1,t)xK1XεK1uLε(Xε,t). Thus, wLε(K1,t)=wLε(Xε,t)=0 for t>0 and wLε(x,t)=0 for K1xXε. In QLεK1={K1<x<Xε,t>0},

    LL0wLε=ruLεXεxXεK1uLεt(K1,t)xK1XεK1uLεt(Xε,t)+(r12σ2L)uLε(Xε,t)uLε(K1,t)XεK1,

    where Li0=t12σi22x2(r12σi2)x. Actually, LL0wLε can be bounded by a number G independent of ε,

    supQLεK1|LL0wLε|rsupQLεK1|uLε|+supQLεK1|uLεt|+2r+σ2LηsupQLεK1|uLε|r+C1+2r+σ2LηG.

    In the case σ2L2r, we introduce the function

    zLε(x,t)=2Cσ2L2r(1exp((12rσ2L)(xXε)))+2Gσ2L2r(xXε),

    where C is a constant to be determined later. Obviously, LL0zLε=GLL0wLε in QLεK1 and zLε(Xε,t)=0 for t>0. To make

    zLεx=2Cσ2Lexp((12rσ2L)(xXε))+2Gσ2L2r0

    hold for K1<x<Xε,t>0, we choose C=σ2LGσ2L2rexp((12rσ2L)(η+ε)). Thus, on the parabolic boundary of QLεK1 we clearly have zLε±wLε. It follows by comparison principle that

    zLε±wLε in QLεK1.

    Since zLε(Xε,t)=±wLε(Xε,t)=0,

    ±(wLε(x,t)wLε(Xε,t))XεxzLε(x,t)zLε(Xε,t)Xεx

    for x<Xε. Letting xXε, we have

    |wLεx(Xε,t)|zLεx(Xε,t)=2Gσ2L2r(1exp((12rσ2L)(η+ε))).

    Then, by uLεx(Xε,t)=wLεx(Xε,t)+[uLε(Xε,t)uLε(K1,t)]/(XεK1) there exists a constant C2>1 independent of ε such that

    |uLεx(Xε,t)|2Gσ2L2r(1exp((12rσ2L)(η+1)))+2/ηC2,

    when ε<1.

    In the case σ2L=2r, we can introduce the function

    zLε(x,t)=Gσ2L(xXε)22Gσ2L(η+ε)(xXε),

    then by a similar analysis as above, we can conclude that there exists a number C2>1 independent of ε such that

    |uLεx(Xε,t)|2Gσ2L(η+1)+2/ηC2,

    when ε<1.

    It is known that uLεx(x,0)=ex for x<0 and uLεx(x,0)=0 for 0<x<Xε. Thus it follows by maximum principle that |uLεx(x,t)|C2 in QLε when ε<1.

    Lemma 3.4.

    |2uLεx2|C4 in QLε¯Qρ, |2uHεx2|C5 in QH. (3.8)

    Proof. The corollary of Lemmas 3.1–3.3.

    In this section, we establish the asymptotic relationship between LL's model and LZ's model, when Xε approaches X. A key lemma is proved to show |uLεxuHεx|0 on x=X along ε0. Then, by compact embedding theorem, we deduce that there exists a subsequence uεj converging a function u which is examined as a solution of the single threshold problem (2.2). By the uniqueness of the solution, we obtain vu and uεv uniformly as ε0.

    Lemma 4.1. As ε0,

    |uLεx(X,t)uHεx(X+,t)|0 (4.1)

    uniformly for 0tT.

    Proof. Let

    hε(t)=uLε(X+ε,t)uLε(X,t)ε=uHε(X+ε,t)uHε(X,t)ε,

    for 0tT. By the mean value theorem, there is μ1(t)[0,ε] such that hε(t)=uLεx(X+μ1(t),t), then,

    |uLεx(X+,t)hε(t)|=|uLεx(X,t)uLεx(X+μ1(t),t)|=|uLεxx(X+μ2(t),t)|μ1(t)εsupQLε¯Qρ|uLεxx|,

    where 0μ2(t)μ1(t). The second equal sign holds by the mean value theorem. Similarly, we can derive

    |uHεx(X+,t)hε(t)|εsupQH|uHεxx|.

    Considering the continuity of uLεx across x=X, we have for 0tT,

    |uLεx(X,t)uHεx(X+,t)|=|uLεx(X+,t)uHεx(X+,t)|=|uLεx(X+,t)hε(t)+hε(t)uHεx(X+,t)|ε(C4+C5).

    As C4,C5 are independent of the small parameter ε, the result is seen by letting ε0.

    Theorem 4.1. As ε0, uε(x,t) tends to v(x,t) uniformly in (,)×[0,T].

    Proof. Treat uLε|xX as uLε restricted on (,X]×[0,T]. From Lemmas 3.1–3.4, uLε|xX is bounded in W2,1((,X)×[0,T]¯Qρ). By the compact embedding theorem, there exists uL and a subsequence εj of ε such that, as εj0,

    uLεj|xXuL in C1+α,1+α2(([A,X]×[0,T])Qρ), 0<α<1, (4.2)

    for any A>1 and ρ<X. Similarly, uHε is bounded in W2,1((X,)×[0,T]) and there exists uH such that

    uHεjuH in C1+α,1+α2([X,A]×[0,T]), (4.3)

    along a subsequence of εj if necessary.

    Thus, it is clear that

    uLεjx(X,t)uLx(X,t), uHεjx(X+,t)uHx(X+,t), (4.4)

    uniformly for 0tT. By Lemma 4.1, we conclude that

    uLx(X,t)=uHx(X+,t). (4.5)

    It then can be verified that u=(uL,uH) is a solution of the problem (2.2). By the uniqueness of the solution to this problem, we have vu. This implies that any convergent subsequence of uLε|xX or uHε has the same limit and uLε|xX or uHε converges as ε0.

    It follows that as ε0,

    uLε(X,t)vL(X,t), uHε(X+,t)vH(X+,t), (4.6)

    uniformly for 0tT. Since uLε(x,0)|xX=vL(x,0) and uHε(x,0)=vH(x,0), implying the maximum norm estimation in their regions, respectively, gives that

    uLε|xXvL uniformly in (,X]×[0,T], (4.7)
    uHεvH uniformly in [X,)×[0,T], (4.8)

    as ε0.

    By PDE techniques, we showed an asymptotic relationship between two kinds of structural models for credit migration problems with fixed boundaries. When the downgrade threshold was locked and the upgrade threshold approached to it, the solution of the model with a pair of asymmetric thresholds converged to that of the single threshold model in which the downgrade threshold serves as a unique migration threshold. Symmetrically, by fixing the upgrade threshold and moving the downgrade threshold, a similar conclusion will be obtained. As far as we know, it was the first time that the relationship between the single threshold and a pair of asymmetric thresholds was studied in credit migration problems. This may contribute to generalizing existing research results by using a single threshold model to approximate models with different upgrade and downgrade thresholds.

    The authors declare they have not used Artificial Intelligence (AI) tools in the creation of this article.

    This work was supported by the National Natural Science Foundation of China (Grant No.12071349).

    All authors declare no conflicts of interest in this paper.



    [1] Feng XD, Chen WC (2016) Research progress of cadmium telluride solar cells. J Nanjing Univ Technol 38: 123–128. https://doi.org/10.3969/j.issn.1671-7627.2016.01.020 doi: 10.3969/j.issn.1671-7627.2016.01.020
    [2] Cheng ZY, Zhu XM, Zeng Y, et al. (2020) Current status of tellurium extraction and utilization. Miner Prot Util 40: 76–89. (in Chines). https://doi.org/10.13779/j.cnki.issn1001-0076.2020.05.010 doi: 10.13779/j.cnki.issn1001-0076.2020.05.010
    [3] Zhang S, Wang XP, Wang LJ, et al. (2010) Research progress of thin film solar cells. Mater Herald 24: 6.
    [4] Yan YF (2015) Latest research progress and challenges in thin film solar cell research. Opt Optoelectron Technol 6: 1–4.
    [5] Li T (1976) Abundance of chemical elements in the Earth. Geochemistry 3: 167–174. (in Chinese)
    [6] Li T, Ni SB (1990) Abundance of chemical elements in the Earth and crust, Beijing: Geological Publishing House, 136. (in Chinese)
    [7] Li T, Yuan HY, Wu SX, et al. (1999) Regional abundance of chemical elements of crust bodies in China. Geotecton Metallog 23: 101–107. (in Chinese)
    [8] Yin JZ, Chen YC, Zhou JX (1995) Introduction of tellurium resources in the world. J Hebei Coll Geol 18: 348–354. (in Chinese)
    [9] Yin JZ (1996) On the paragenetic model and mineralizing mechanism of the Dashuigou independent tellurium deposit in Shimian County, Sichuan Province, China-the only independent tellurium deposit in the world, Chongqing: Chongqing Publishing House, 190. (in Chinese)
    [10] Yin JZ, Shi HY (2020) Mineralogy and stable isotopes of tetradymite from the Dashuigou tellurium deposit, Tibet Plateau, southwest China. Sci Rep 10: 4634. https://doi.org/10.1038/s41598-020-61581-3 doi: 10.1038/s41598-020-61581-3
    [11] Tu GC, Gao ZM, Hu RZ, et al. (2004) Dispersed element geochemistry and mineralization mechanism, Beijing: Geological Publishing House, 430.
    [12] Nassar NT, Kim H, Frenzel M, et al. (2022) Global tellurium supply potential from electrolytic copper refining. Resour Conserv Recycl 184: 106434. https://doi.org/10.1016/j.resconrec.2022.106434 doi: 10.1016/j.resconrec.2022.106434
    [13] Wedepohl KH (1995) The composition of the continental crust. Geochim Cosmochim Acta 59: 1217–1232. https://doi.org/10.1016/0016-7037(95)00038-2 doi: 10.1016/0016-7037(95)00038-2
    [14] Yin JZ, Shi HY (2021) Fluid inclusions and metallogenic conditions of the Dashuigou tellurium deposit, Tibet Plateau, southwest China. Geol Earth Mar Sci 3: 1–15. https://doi.org/10.31038/GEMS.2021331 doi: 10.31038/GEMS.2021331
    [15] Qian HD, Chen W, Xie JD, et al. (2000) Tellurium mineral review. J Geol Univer 6: 178–187. https://doi.org/10.3969/j.issn.1006-7493.2000.02.011 doi: 10.3969/j.issn.1006-7493.2000.02.011
    [16] Shao J, Tao WP (2014) Mineral Resources Industry Requirements Manual, Beijing: Geological Publishing House, 952.
    [17] Hu XL, Yao SZ, He MZ, et al. (2021) An Overview of Advances in Tellurium Mineralization in Telluride-Rich Gold Deposits. Earth Sci 46: 3807–3817. https://doi.org/10.3799/dqkx.2021.002 doi: 10.3799/dqkx.2021.002
    [18] Wang XM, Sun ZX (2009) Production status and development prospects of selenium and tellurium. China Nonferrous Metall, 38–43. https://doi.org/10.3969/j.issn.1672-6103.2009.01.011 doi: 10.3969/j.issn.1672-6103.2009.01.011
    [19] Xing X, Guo JQ (2009) Application of tellurium and its resource distribution. Miner Prot Util, 19–22. https://doi.org/10.3969/j.issn.1001-0076.2009.03.005 doi: 10.3969/j.issn.1001-0076.2009.03.005
    [20] Jiang HL, Dai T (2016) Analysis and suggestions of tellurium's supply and demand of China in the future. China Mining 25: 7–10. https://doi.org/10.3969/j.issn.1004-4051.2016.10.002 doi: 10.3969/j.issn.1004-4051.2016.10.002
    [21] USGS, Selenium and Tellurium Statistics and Information. Natiuonal Mineral Informatiuon Center, 2023. Available from: https://www.usgs.gov/centers/national-minerals-information-center/selenium-and-tellurium-statistics-and-information.
    [22] USGS, Tellurium. 2003. Available from: https://pubs.usgs.gov/periodicals/mcs2023/mcs2023-tellurium.pdf.
    [23] Goldfarb RJ, Berger BR, George MW, et al. (2017) Tellurium, Critical Mineral Resources of the United States-Economic and Environmental Geology and Prospects for Future Supply, U.S. Geological Survey Professional Paper 1802, R1–R27.
    [24] Zhao T, Liu C (2018) Atlas of Three Rare Resources at Home and Abroad, Beijing: Geological Press.
    [25] Xiao P, Wang HJ, Ye FC, et al. (2020) Current status and prospects of recovery technology of scattered metal selenium and tellurium. Met Min 4: 52–60. https://doi.org/10.19614/j.cnki.jsks.202004009 doi: 10.19614/j.cnki.jsks.202004009
    [26] Liu JJ, Zhai DG, Wang DZ, et al. (2020) Au-(Ag)-Te-Se mineralization system and mineralization. Geosci Front 27: 79–98.
    [27] Chen YC, Mao JW, Zhou JX, et al. (1993) Dashuigou tellurium gold deposit in Shimian County, Sichuan Province—the world's first independent tellurium deposit mainly composed of tellurium. Proceedings of the Fifth National Conference on Mineral Deposits, Beijing: Geological Publishing House, 437–439. (in Chinese)
    [28] Luo YN, Cao ZM (1994) The world's first independent tellurium deposit was discovered in Sichuan Province. China Geol, 27–28. (in Chines)
    [29] Yin JZ, Xiang SP, Chao YH, et al. (2022) Petrochemical eigenvalues and diagrams for the identification of metamorphic rocks' protolith, taking the host rocks of Dashuigou tellurium deposit in China as an example. Acta Geochim 42: 103–124. https://doi.org/10.1007/s11631-022-00583-6 doi: 10.1007/s11631-022-00583-6
    [30] Luo YN, Fu DM, Zhou SD (1994) Genesis of the Dashuigou tellurium deposit in Sichuan Province of China. Bull Sichuan Geol 14: 101–110. (in Chines)
    [31] Cao ZM, Luo YN (1993) Geological characteristics and material composition of the Shimian Te (Se) deposit in Sichuan Province. Proceedings of the Fifth National Conference on Mineral Deposits, Beijing: Geological Publishing House, 476–476. (in Chinese)
    [32] Yin JZ, Zhou JX, Yang BC (1994) Rock-forming minerals and ore-forming minerals of the Dashuigou tellurium ore deposit unique in the world—A preliminary study. Sci Geol Sinica 3: 197–210.
    [33] Yin JZ, Chen YC, Zhou JX (1994) Mineralogical research of the Dashuigou independent tellurium deposit in Sichuan Province, China. Bull Mineral Petrol Geochem 3: 153–155. (in Chinese)
    [34] Yin JZ, Zhou JX, Yang BC (1994) Geological characteristics of the Dashuigou tellurium deposit in Sichuan Province, China. Earth Sci Front 1: 241–243. (in Chinese)
    [35] Chen YC, Yin, JZ, Zhou JX (1994) The first and only independent tellurium ore deposit in Dashuigou, Shimian County, Sichuan Province, China. Sci Geol Sinica 3: 109–113. (in Chinese)
    [36] Chen YC, Yin JZ, Zhou JX (1994) Geology of the Dashuigou independent tellurium deposit of Sichuan Province. Acta Geoscientia Sinica 29: 165–167. (in Chinese)
    [37] Cao ZM, Luo YN (1994) Mineral sequence and ore genesis of the Sichuan telluride lode deposit in China. New Research Progresses of the Mineralogy, Petrology and Geochemistry in China. Lanzhou: Lanzhou University Publishing House, 476–478. (in Chinese)
    [38] Luo YN, Fu DM, Zhou SD, et al. (1994) Geology and genesis of the Dashuigou tellurium deposit in Shimian County, Sichuan Province. Sichuan Geol J 14: 1–10. (in Chinese)
    [39] Yin JZ, Chen YC, Zhou JX (1995) The metallogenic age of the world's first independent tellurium deposit. Chin Sci Bull 40: 766–767. (in Chinese)
    [40] Yin JZ, Chen YC, Zhou JX (1995) K-Ar isotope evidence for age of the first and only independent tellurium deposit. Chin Sci Bull 22: 1933–1934.
    [41] Yin JZ, Chen YC, Zhou JX (1995) Original rock of the host rock of the Dashuigou independent tellurium deposit in Sichuan Province, China. Bull Mineral Petrol Geochem, 114–115. (in Chinese)
    [42] Cao ZM, Wen CQ, Li BH (1995) Genesis of the Dashuigou tellurium deposit in Sichuan Province of China. Sci China B 25: 647–654. (in Chinese)
    [43] Wang RC, Shen WZ, Xu XJ, et al.(1995)Isotopic geology of the Dashuigou tellurium deposit in Sichuan Province, China. J Nanjing Univ (Natural Sciences) 31: 617–624. (in Chinese)
    [44] Mao JW, Chen YC, Zhou JX (1995) Geology, mineralogy, petrology, and geochemistry of the Dashuigou tellurium deposit in Shimian County, Sichuan Province, China. Acta Geosci 2: 276–290. (in Chinese)
    [45] Yin JZ (1996) The paragenetic model and mineralizing mechanism of the Dashuigou independent tellurium deposit in Shimian County, Sichuan—the first and only independent tellurium deposit in the world. Acta Geoscientia Sinica, 93–97.
    [46] Yin JZ, Chen YC, Zhou JX (1996) Geology and geochemistry of host rocks of the Dashuigou independent tellurium deposit in Sichuan Province, China. J Changchun Univ Earth Sci 26: 322–326. (in Chinese)
    [47] Yin JZ, Chen YC, Zhou JX (1996) Geology and geochemistry of altered rocks of the Dashuigou independent tellurium deposit in Sichuan Province, China. J Xi'an Coll Geol 18: 19–25. (in Chinese)
    [48] Luo YN, Cao ZM, Wen CQ (1996) Geology of the Dashuigou independent tellurium deposit, Chengdu: Southwest Communication University Publishing House, 30–45. (in Chinese)
    [49] Chen YC, Mao JW, Luo YN, et al. (1996) Geology and Geochemistry of the Dashuigou tellurium (gold) deposit in Western Sichuan, China, Beijing: Atomic Energy Press, 146. (in Chinese)
    [50] Wang RC, Chen XM, Xu SJ (1996) Complex exsolution of tellurium minerals in the Dashuigou tellurium deposit. Sci Bull 41: 920–922.
    [51] Liu AP, Zhong ZC, Tang JW (1996) Geochemical characteristics of the Dashuigou tellurium deposit in Sichuan Province of China. Geochemistry 25: 365–371. (in Chinese)
    [52] Chen PR, Lu JJ, Wang RC, et al. (1998) Study on the fluid inclusions of the Dashuigou independent tellurium deposit in Shimian County, Sichuan Province, China. Miner Deposit 17: 1011–1014. (in Chinese)
    [53] Yin JZ, Shi HY (2019) Nano effect mineralization of rare elements--taking the Dashuigou tellurium deposit, Tibet Plateau, Southwest China as the example. Acad J Sci Res 7: 635–642. https://doi.org/10.15413/ajsr.2019.0902 doi: 10.15413/ajsr.2019.0902
    [54] Wang RC, Lu JJ, Chen XM (2000) Genesis of the Dashuigou tellurium deposit in Sichuan Province, China. Bull Mineral Petrol Geochem 4: 348–349. (in Chinese)
    [55] Xu ZQ, Hou LW, Wang ZX, et al. (1992) The orogenic process of the Songpan-Ganzi orogenic belt in China, Beijing: Geological Publishing House, 190. (in Chinese)
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