Qeyri-bircins mühitin tektonik maqnit-paleomaqnit xəritələnməsi: onun Şərqi Aralıq dənizi (Şimali İsrail) ərazisi üçün əhəmiyyəti
Lev Eppelbaum1,2, Yuriy Kats2
1 Tel-Əviv Universitetinin dəqiq elmlər fakültəsi, geofizika kafedrası İsrail, Tel-Aviv, Ramat-Aviv 6997801
2 Azərbaycan Dövlət Neft və Sənaye Universiteti Azadlıq pr. 20, Bakı, AZ 1010, Azərbaycan
3 Təbii Tarix muzeyi və Şteynqartd milli tədqiqat mərkəzi, Tel-Əviv Universitetinin Təbiət elmləri fakültəsi İsrail, Tel-Aviv, Ramat-Aviv 6997801
Xülasə
Okeandan kontinent zonasına keçid, həmçinin cpredinq və litosfer plitələrinin qovuşma məkanları Yerin geoloji baxımdan ən mürəkkəb regionlarındandır. Yerin ən böyük: Avroasiya və hondvana litosfer plitələrin qovşağında yerləşmiş Şərqi Aralıq dəniz ərazisi bu deyilənlərə parlaq nümunədir. Maqnit anomaliyalarının kəmiyyət analizi mürəkkəb relyefin maili maqnitləşmə (1) və müxtəlif dərəcəli anomaliyaların üstə-üstə düşməsi şəraitlərində interpretasiya əməliyatları tətbiq etməyə imkan verən qabaqcıl metodikalardan istifadə etməklə yerinə yetirilmişdir. İsrailin şimalında – Qaliley dənizi, Karmelan və Malkişon kimi bir neçə mürəkkəb geoloji rayonların maqnit anomaliyalarının dəqiq analizi nümunələri təqdim olunmuşdur. Belə keçid zonalarının paleomaqnit xəritələnməsinin metodu həm kontinental, həm də okean platformalarının paleomaqnit rekonstruksiyaları, maqnitoaktiv süxurların radiometrikliyinin qeydiyyat nəticələri, peyk məlumatlarının öyrənilməsi, tektonik-struktur rekonstruktursiyalar, biocoğrafi təhlil və müxtəlif geofiziki tədqiqat nəticələrinin istifadəsinə, xəritələmə metodlarının kompleksləşdirilməsinə əsaslanmışdır. Geodinamik paleomaqnit xəritələmə nəinki mühitin çoxsəviyyəli struktur qeyri-bircinsliyini, həmçinin qovuşma (keçid) zonalarına xas olan müxtəlif yaşlı geodinamikanın mürəkkəb elementlərini əksetdirməyə imkan verir. İsraildə kompleks paleomaqnit xəritələnməsi üçün paleomaqnit və radiometrik metodlarla (həmçinin struktur-tektonik üsullarla) öyrənilmiş rayonlar seçilmişdir: 1) ətraf zonalarla (əvvəllər bu rayonların qurulmuş sxemləri korrektə edilmiş və əlavələr edilmiş) birlikdə Qaliley dənizi, 2) Karmel rayonu və 3) Atlit rayonu (Karmel rayonunun daxili hissəsi) Karmel rayonu üçün Alt təbaşir traplarının akkumulyativ səthinin tavanı üzrə qurulmuş paleomaqnit profil regionun paleogeodinamik inkişaf tarixinin mürəkkəbliyini bariz şəkildə nümayiş etdirir. Mürəkkəb mühitlərin paleomaqnit xəritələnməsilə yanaşı maqnit anomaliyalarının kəmiyyətcə interpretasiya əməliyyatlarının birlikdə aparılmasının effektivliyi haqqında nəticə çıxarılmışdır. 3.6-2.0 mln il əvvəlki dövr üçün işlənilmiş palinspatik rekonstruksiya bu geoloji zaman kəsiyinin mühüm tektonik-maqmatik xüsusiyyətlərinin aşkarlanmasına imkan verir.
Açar sözlər: paleomaqnit xəritələmə, paleomaqnit profilləmə, maqnit məlumatlarının təhlili, tektonik-struktur interpretasiya, kompleks analiz, palinspatik rekonstruksiya
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DOI: 10.33677/ggianas20220200079