Review Special Issues

Processing and interpretation of magnetic data in the Caucasus Mountains and the Caspian Sea: A review

  • Received: 28 March 2024 Revised: 21 April 2024 Accepted: 06 May 2024 Published: 14 May 2024
  • With the rapid development of aeromagnetic (primarily uncrewed) methods for measuring the magnetic field, the possibility of detailed magnetic research in hard-to-reach mountainous areas, forested areas, swamp areas, desert areas, and water areas has emerged. The conditions for interpreting the magnetic field are most difficult due to the vector nature of the magnetic properties of rocks, the wide range of their properties, and the presence of residual magnetization. The physical and geological conditions of the territory of Azerbaijan are characterized by rugged terrain relief, inclined magnetization (~58°), and complex geological environments. Along with using a probabilistic approach, deterministic methods for solving inverse and direct problems of geophysics become of great importance since it is possible to identify relatively extended reference boundaries and analyze magnetic anomalies from separate bodies of relatively simple shape. The article briefly outlines the main stages of processing and interpreting magnetic data under complex environments. The theoretical examples discussed include a block diagram of various disturbances, interpretive models of thin and thick beds, an intermediate model, a thin horizontal plate, and a horizontal circular cylinder on the flat and inclined surfaces under inclined magnetization conditions. The process of assessing magnetization on sloping terrain relief is shown. The presented field examples for the Caucasus Mountains show the quantitative interpretation of aeromagnetic data at the Big Somalit and Guton sites (southern Greater Caucasus, Azerbaijan), a deep regional profile through the Lesser and Greater Caucasus, magnetic field studies in the area around the Saatly superdeep borehole (Middle Kur depression between the Greater and Lesser Caucasus), and 3D magnetic field modeling at the Gyzylbulag gold deposit (the Azerbaijani part of the Lesser Caucasus). In the Caspian Sea, we demonstrated the use of an information parameter to identify faults in the Bulla hydrocarbon field (Gulf of Baku) and, for the first time, obtained the relationship between the generalized aeromagnetic data (2.5 kilometers over the mean sea level) and the central area of the mud volcanoes distribution in Azerbaijan.

    Citation: Lev Eppelbaum. Processing and interpretation of magnetic data in the Caucasus Mountains and the Caspian Sea: A review[J]. AIMS Geosciences, 2024, 10(2): 333-370. doi: 10.3934/geosci.2024019

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  • With the rapid development of aeromagnetic (primarily uncrewed) methods for measuring the magnetic field, the possibility of detailed magnetic research in hard-to-reach mountainous areas, forested areas, swamp areas, desert areas, and water areas has emerged. The conditions for interpreting the magnetic field are most difficult due to the vector nature of the magnetic properties of rocks, the wide range of their properties, and the presence of residual magnetization. The physical and geological conditions of the territory of Azerbaijan are characterized by rugged terrain relief, inclined magnetization (~58°), and complex geological environments. Along with using a probabilistic approach, deterministic methods for solving inverse and direct problems of geophysics become of great importance since it is possible to identify relatively extended reference boundaries and analyze magnetic anomalies from separate bodies of relatively simple shape. The article briefly outlines the main stages of processing and interpreting magnetic data under complex environments. The theoretical examples discussed include a block diagram of various disturbances, interpretive models of thin and thick beds, an intermediate model, a thin horizontal plate, and a horizontal circular cylinder on the flat and inclined surfaces under inclined magnetization conditions. The process of assessing magnetization on sloping terrain relief is shown. The presented field examples for the Caucasus Mountains show the quantitative interpretation of aeromagnetic data at the Big Somalit and Guton sites (southern Greater Caucasus, Azerbaijan), a deep regional profile through the Lesser and Greater Caucasus, magnetic field studies in the area around the Saatly superdeep borehole (Middle Kur depression between the Greater and Lesser Caucasus), and 3D magnetic field modeling at the Gyzylbulag gold deposit (the Azerbaijani part of the Lesser Caucasus). In the Caspian Sea, we demonstrated the use of an information parameter to identify faults in the Bulla hydrocarbon field (Gulf of Baku) and, for the first time, obtained the relationship between the generalized aeromagnetic data (2.5 kilometers over the mean sea level) and the central area of the mud volcanoes distribution in Azerbaijan.



    Over the last two decades, many researches used LKF method to get stability results for time-delay systems [1,2]. The LKF method has two important technical steps to reduce the conservatism of the stability conditions. The one is how to construct an appropriate LKF, and the other is how to estimate the derivative of the given LKF. For the first one, several types of LKF are introduced, such as integral delay partitioning method based on LKF [3], the simple LKF [4,5], delay partitioning based LKF [6], polynomial-type LKF [7], the augmented LKF [8,9,10]. The augmented LKF provides more freedom than the simple LKF in the stability criteria because of introducing several extra matrices. The delay partitioning based LKF method can obtain less conservative results due to introduce several extra matrices and state vectors. For the second step, several integral inequalities have been widely used, such as Jensen inequality [11,12,13,14], Wirtinger inequality [15,16], free-matrix-based integral inequality [17], Bessel-Legendre inequalities [18] and the further improvement of Jensen inequality [19,20,21,22,23,24,25]. The further improvement of Jensen inequality [22] is less conservative than other inequalities. However, The interaction between the delay partitioning method and the further improvement of Jensen inequality [23] was not considered fully, which may increase conservatism. Thus, there exists room for further improvement.

    This paper further researches the stability of distributed time-delay systems and aims to obtain upper bounds of time-delay. A new LKF is introduced via the delay partitioning method. Then, a less conservative stability criterion is obtained by using the further improvement of Jensen inequality [22]. Finally, an example is provided to show the advantage of our stability criterion. The contributions of our paper are as follows:

    The integral inequality in [23] is more general than previous integral inequality. For r=0,1,2,3, the integral inequality in [23] includes those in [12,15,21,22] as special cases, respectively.

    An augmented LKF which contains general multiple integral terms is introduced to reduce the conservatism via a generalized delay partitioning approach. For example, the tt1mhx(s)ds, tt1mhtu1x(s)dsdu1, , tt1mhtu1tuN1x(s)dsduN1du1 are added as state vectors in the LKF, which may reduce the conservatism.

    In this paper, a new LKF is introduced based on the delay interval [0,h] is divided into m segments equally. From the LKF, we can conclude that the relationship among x(s), x(s1mh) and x(sm1mh) is considered fully, which may yield less conservative results.

    Notation: Throughout this paper, Rm denotes m-dimensional Euclidean space, A denotes the transpose of the A matrix, 0 denotes a zero matrix with appropriate dimensions.

    Consider the following time-delay system:

    ˙x(t)=Ax(t)+B1x(th)+B2tthx(s)ds, (2.1)
    x(t)=Φ(t),t[h,0], (2.2)

    where x(t)Rn is the state vector, A,B1,B2Rn×n are constant matrices. h>0 is a constant time-delay and Φ(t) is initial condition.

    Lemma2.1. [23] For any matrix R>0 and a differentiable function x(s),s[a,b], the following inequality holds:

    ba˙xT(s)R˙x(s)dsrn=0ρnbaΦn(a,b)TRΦn(a,b), (2.3)

    where

    ρn=(nk=0cn,kn+k+1)1,
    cn,k={1,k=n,n0,n1t=kf(n,t)ct,k,k=0,1,n1,n1,
    Φl(a,b)={x(b)x(a),l=0,lk=0cl,kx(b)cl,0x(a)lk=1cl,kk!(ba)kφk(a,b)x(t),l1,
    f(l,t)=tj=0ct,jl+j+1/tj=0ct,jt+j+1,
    φk(a,b)x(t)={bax(s)ds,k=1,babs1bsk1x(sk)dskds2dss1,k>1.

    Remark2.1. The integral inequality in Lemma 2.1 is more general than previous integral inequality. For r=0,1,2,3, the integral inequality (2.3) includes those in [12,15,21,22] as special cases, respectively.

    Theorem3.1. For given integers m>0,N>0, scalar h>0, system (2.1) is asymptotically stable, if there exist matrices P>0, Q>0, Ri>0,i=1,2,,m, such that

    Ψ=ξT1Pξ2+ξT2Pξ1+ξT3Qξ3ξT4Qξ4+mi=1(hm)2ATdRiAdmi=1rn=0ρnωn(timh,ti1mh)Ri×ωn(timh,ti1mh)<0, (3.1)

    where

    ξ1=[eT1ˉET0ˉET1ˉET2ˉETN]T,
    ξ2=[ATdET0ET1ET2ETN]T,
    ξ3=[eT1eT2eTm]T,
    ξ4=[eT2eT3eTm+1]T,
    ˉE0=hm[eT2eT3eTm+1]T,
    ˉEi=hm[eTim+2eTim+3eTim+m+1]T,i=1,2,,N,
    Ei=hm[eT1eTim+2eT2eTim+3eTmeTm(i+1)+1]T,i=0,1,2,,N,
    Ad=Ae1+B1em+1+B2mi=0em+1+i,
    ωn(timh,ti1mh)={eiei+i,n=0,nk=0cn,keicn,0ei+1nk=1cn,kk!e(k1)m+k+1,n1,
    ei=[0n×(i1)nIn×n0n×(Nm+1i)]T,i=1,2,,Nm+1.

    Proof. Let an integer m>0, [0,h] can be decomposed into m segments equally, i.e., [0,h]=mi=1[i1mh,imh]. The system (2.1) is transformed into

    ˙x(t)=Ax(t)+B1x(th)+B2mi=1ti1mhtimhx(s)ds. (3.2)

    Then, a new LKF is introduced as follows:

    V(xt)=ηT(t)Pη(t)+tthmγT(s)Qγ(s)ds+mi=1hmi1mhimhtt+v˙xT(s)Ri˙x(s)dsdv, (3.3)

    where

    η(t)=[xT(t)γT1(t)γT2(t)γTN(t)]T,
    γ1(t)=[tt1mhx(s)dst1mht2mhx(s)dstm1mhthx(s)ds],γ2(t)=mh[tt1mhtu1x(s)dsdu1t1mht2mht1mhu1x(s)dsdu1tm1mhthtm1mhu1x(s)dsdu1],,
    γN(t)=(mh)N1×[tt1mhtu1tuN1x(s)dsduN1du1t1mht2mht1mhu1t1mhuN1x(s)dsduN1du1tm1mhthtm1mhu1tm1mhuN1x(s)dsduN1du1],
    γ(s)=[x(s)x(s1mh)x(sm1mh)].

    The derivative of V(xt) is given by

    ˙V(xt)=2ηT(t)P˙η(t)+γT(t)Qγ(t)γT(thm)Qx(thm)+mi=1(hm)2˙xT(t)Ri˙x(t)mi=1hmti1mhtimh˙xT(s)Ri˙x(s)ds.

    Then, one can obtain

    ˙V(xt)=ϕT(t){ξT1Pξ2+ξT2Pξ1+ξT3Qξ3ξT4Qξ4+mi=1(hm)2ATdRiAd}ϕ(t)mi=1hmti1mhtimh˙xT(s)Ri˙x(s)ds, (3.4)
    ϕ(t)=[xT(t)γT0(t)γT1(t)γTN(t)]T,
    γ0(t)=[xT(t1mh)xT(t2mh)xT(th)]T.

    By Lemma 2.1, one can obtain

    hmti1mhtimh˙xT(s)Ri˙x(s)dsrl=0ρlωl(timh,ti1mh)Ri×ωl(timh,ti1mh). (3.5)

    Thus, we have ˙V(xt)ϕT(t)Ψϕ(t) by (3.4) and (3.5). We complete the proof.

    Remark3.1. An augmented LKF which contains general multiple integral terms is introduced to reduce the conservatism via a generalized delay partitioning approach. For example, the tt1mhx(s)ds, tt1mhtu1x(s)dsdu1, , tt1mhtu1tuN1x(s)dsduN1du1 are added as state vectors in the LKF, which may reduce the conservatism.

    Remark3.2. For r=0,1,2,3, the integral inequality (3.5) includes those in [12,15,21,22] as special cases, respectively. This may yield less conservative results. It is worth noting that the number of variables in our result is less than that in [23].

    Remark3.3. Let B2=0, the system (2.1) can reduces to system (1) with N=1 in [23]. For m=1, the LKF in this paper can reduces to LKF in [23]. So the LKF in our paper is more general than that in [23].

    This section gives a numerical example to test merits of our criterion.

    Example 4.1. Consider system (2.1) with m=2,N=3 and

    A=[011001],B1=[0.00.10.10.2],B2=[0000].

    Table 1 lists upper bounds of h by our methods and other methods in [15,20,21,22,23]. Table 1 shows that our method is more effective than those in [15,20,21,22,23]. It is worth noting that the number of variables in our result is less than that in [23]. Furthermore, let h=1.141 and x(0)=[0.2,0.2]T, the state responses of system (1) are given in Figure 1. Figure 1 shows the system (2.1) is stable.

    Table 1.  hmax for different methods.
    Methods hmax NoDv
    [15] 0.126 16
    [20] 0.577 75
    [21] 0.675 45
    [22] 0.728 45
    [23] 0.752 84
    Theorem 3.1 1.141 71
    Theoretical maximal value 1.463

     | Show Table
    DownLoad: CSV
    Figure 1.  The state trajectories of the system (2.1) of Example 4.1.

    In this paper, a new LKF is introduced via the delay partitioning method. Then, a less conservative stability criterion is obtained by using the further improvement of Jensen inequality. Finally, an example is provided to show the advantage of our stability criterion.

    This work was supported by Basic Research Program of Guizhou Province (Qian Ke He JiChu[2021]YiBan 005); New Academic Talents and Innovation Program of Guizhou Province (Qian Ke He Pingtai Rencai[2017]5727-19); Project of Youth Science and Technology Talents of Guizhou Province (Qian Jiao He KY Zi[2020]095).

    The authors declare that there are no conflicts of interest.



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