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Tektonik qurulu艧 - Azerbaijan.az

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22.062 22.062; margin: 0 7px -4px 7px;" xml:space="preserve"><g> <path d="M17.294,9.443L8.459,0.608c-0.812-0.811-2.138-0.811-2.945,0L4.775,1.345c-0.81,0.81-0.81,2.136,0,2.944l6.742,6.743 l-6.742,6.741c-0.81,0.811-0.81,2.137,0,2.943l0.737,0.737c0.81,0.811,2.136,0.811,2.945,0l8.835-8.836 c0.435-0.435,0.628-1.018,0.597-1.589C17.922,10.46,17.729,9.877,17.294,9.443z" fill="#931933"/> </g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g> </svg> <h2 class="info-second-title"> <a href="/information/203">Geoloji qurulu艧</a> </h2> <svg xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink" version="1.1" id="Capa_1" x="0px" y="0px" width="12px" height="12px" viewBox="0 0 22.062 22.062" style="enable-background:new 0 0 22.062 22.062; margin: 0 7px -1px 7px;" xml:space="preserve"><g> <path d="M17.294,9.443L8.459,0.608c-0.812-0.811-2.138-0.811-2.945,0L4.775,1.345c-0.81,0.81-0.81,2.136,0,2.944l6.742,6.743 l-6.742,6.741c-0.81,0.811-0.81,2.137,0,2.943l0.737,0.737c0.81,0.811,2.136,0.811,2.945,0l8.835-8.836 c0.435-0.435,0.628-1.018,0.597-1.589C17.922,10.46,17.729,9.877,17.294,9.443z" fill="#931933"/> </g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g><g></g> </svg> <h3 class='info-third-title'> Tektonik qurulu艧 </h3> <ul class="list"> <li class=''><a href="/information/201">脺mumi m蓹lumat</a></li> <li class=''><a href="/information/202">Relyef</a></li> <li class='active'><a href="/information/203">Geoloji qurulu艧</a></li> <li class=''><a href="/information/204">陌qlim</a></li> <li class=''><a href="/information/205">Bitki 枚rt眉y眉</a></li> <li class=''><a href="/information/206">Heyvanlar al蓹mi</a></li> <li class=''><a href="/information/207">X蓹z蓹r d蓹nizi</a></li> <li class=''><a href="/information/208">Daxili sular</a></li> <li class=''><a href="/information/209">Ekologiya v蓹 t蓹bi蓹tin m眉hafiz蓹si</a></li> </ul> <ul class="list sublist"> <li class='active'><a href="/related-information/236">Tektonik qurulu艧</a></li> <li class=''><a href="/related-information/12">Faydal谋 qaz谋nt谋lar</a></li> <li class=''><a href="/related-information/13">Yeralt谋 sular</a></li> <li class=''><a href="/related-information/14">Pal莽谋q vulkanlar谋</a></li> <li class=''><a href="/related-information/15">Seysmiklik</a></li> </ul> </section> <section class="section article"> <article> <div id="titlebox" style="margin: 0px; overflow: hidden; display: table; width: 550px; height: 14px; padding-top: 10px; color: rgb(70, 70, 70); font-family: Tahoma; font-size: 12px;"> <div id="titlename" style="margin: 0px; overflow: hidden; color: rgb(43, 43, 43); font-variant-numeric: normal; font-variant-east-asian: normal; line-height: normal; font-stretch: normal; height: 100%; width: 500px; padding-left: 3px; font-weight: bold; display: inline; text-align: justify;"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">TEKTON陌K QURULU艦</span></span></div> </div> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">Az蓹rbaycan Respublikas谋n谋n 蓹razisi geoloji c蓹h蓹td蓹n Alp q谋r谋艧谋ql谋q qur艧a臒谋na daxildir. B&ouml;y&uuml;k v蓹 Ki&ccedil;ik Qafqaz谋n c蓹nub-艧蓹rq hiss蓹l蓹rini v蓹 onlar谋 ay谋ran K&uuml;r da臒aras谋 &ccedil;&ouml;k蓹kliyini, h蓹m&ccedil;inin Orta X蓹z蓹r v蓹 C蓹nubi X蓹z蓹r &ccedil;&ouml;k蓹klikl蓹rini 蓹hat蓹 ed蓹n&nbsp;</span></span><img alt="" src="https://azerbaijan.az/uploads/news-files/melumatlar/relyef-oroqrafiya/DSC_0054.jpg" style="float:right; font-family:arial,helvetica,sans-serif; font-size:14px; height:399px; margin:10px; text-align:justify; width:600px" /><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">m&uuml;xt蓹lif&nbsp;qurulu艧lu q谋r谋艧谋q sisteml蓹rd蓹n ibar蓹tdir. Az蓹rbaycan Respublikas谋nda Yer qab谋臒谋n谋n qal谋nl谋臒谋 38-55 km aras谋nda d蓹yi艧ir. Maksimum qal谋nl谋臒谋 B&ouml;y&uuml;k Qafqaz 蓹razisind蓹, minimum qal谋nl谋臒谋 Tal艧谋n 蓹t蓹kl蓹rind蓹dir. 茝razinin geoloji qurulu艧unda &ccedil;&ouml;km蓹, vulkanogen-&ccedil;&ouml;km蓹, vulkanogen v蓹 kontinental s&uuml;xurlardan t蓹艧kil olunmu艧 Kembrid蓹n 蓹vv蓹lki d&ouml;vrd蓹n ba艧layaraq m&uuml;asir d&ouml;vr &ccedil;&ouml;k&uuml;nt&uuml;l蓹ri daxil olmaqla b&uuml;t&uuml;n geoloji d&ouml;vrl蓹rin &ccedil;&ouml;k&uuml;nt&uuml; kompleksl蓹ri i艧tirak edir. Respublikada 蓹n &ccedil;ox Mezozoy v蓹 h蓹m&ccedil;inin Kaynozoy ya艧l谋 evgeosinklinal, miogeosinklinal v蓹 molass &ccedil;&ouml;k&uuml;nt&uuml;l蓹r yay谋lm谋艧d谋r. Az sah蓹d蓹 Paleozoyun subplatforma &ccedil;&ouml;k&uuml;nt&uuml;l蓹ri v蓹 Alp Paleozoy-Kembrid蓹n &ouml;nc蓹ki metamorfik s&uuml;xurlar var.</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">Az蓹rbaycan Respublikas谋n谋n 蓹sas struktur vahidl蓹ri B&ouml;y&uuml;k Qafqaz meqantiklinoriumu, K&uuml;r da臒laras谋 &ccedil;&ouml;k蓹kliyi v蓹 Ki&ccedil;ik Qafqaz meqantiklinoriumdur.</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">B&ouml;y&uuml;k Qafqaz meqantiklinoriumu m&uuml;r蓹kk蓹b qurulu艧lu struktur olub, daxilind蓹 q蓹dim strukturlarla yana艧谋, cavan t&ouml;r蓹m蓹 strukturlar da yerl蓹艧ir:</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">B&ouml;y&uuml;k Qafqaz antiklinoriumunun t蓹svir edil蓹n b&uuml;t&uuml;n strukturlar谋 Girdiman &ccedil;ay谋nda k蓹skin bataraq, 艧蓹rqd蓹 X蓹z蓹r sahill蓹rind蓹 periklinal 艧蓹klind蓹 qapan谋r. 艦amax谋-Qobustan sinklinoriumu sah蓹sind蓹 V蓹ndam antiklinoriumunun g&ouml;m&uuml;lm&uuml;艧 davam谋 Yavan谋da臒-Sanqa&ccedil;al a臒谋rl谋q q&uuml;vv蓹si maksimumu hesab edilir. Burada, Girdiman v蓹 A臒su &ccedil;aylar谋 aras谋nda Maykop &ccedil;&ouml;k&uuml;nt&uuml;l蓹ri &uuml;z蓹rind蓹 qal谋n (1500 m) D&uuml;brar fasiyal谋 Taba艧ir &ccedil;&ouml;k&uuml;nt&uuml;l蓹ri &ouml;rt&uuml;y&uuml; (horizontal yerd蓹yi艧m蓹 amplitudu 10 km) yerl蓹艧ir ki, bu da Basqal &ouml;rt&uuml;y&uuml; adlan谋r. Q蓹rbd蓹 Maz谋m v蓹 Girdiman &ccedil;aylar谋 aras谋nda V蓹ndam antiklinoriumunun xeyli c蓹nub hiss蓹si &ccedil;aq谋l da艧lar谋 il蓹 &ouml;rt&uuml;lm&uuml;艧d&uuml;r.</span></span></p> <p><img alt="" src="https://azerbaijan.az/uploads/news-files/melumatlar/relyef-oroqrafiya/az%C9%99rbaycan.jpg" style="float:left; font-family:arial,helvetica,sans-serif; font-size:14px; height:450px; margin:10px; text-align:justify; width:600px" /></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">K&uuml;r da臒aras谋 &ccedil;&ouml;k蓹kliyi uzun geoloji vaxt 蓹rzind蓹 formala艧m谋艧d谋r. Lakin m&uuml;asir konfiqurasiyas谋n谋 yaln谋z Oliqosen &mdash; d&ouml;rd&uuml;nc&uuml; d&ouml;vrd蓹 alm谋艧d谋r. &Ccedil;&ouml;k蓹kliyin b&uuml;n&ouml;vr蓹sind蓹 uzununa istiqam蓹td蓹 q蓹rbd蓹n 艧蓹rq蓹 v蓹 h蓹m&ccedil;inin 艧imaldan c蓹nuba v蓹 蓹ksin蓹 pill蓹li enm蓹 m&uuml;艧ahid蓹 edilir. &Ccedil;&ouml;k蓹klik t&ouml;r蓹m蓹 struktur olub, &uuml;std蓹 yatan &ccedil;&ouml;k&uuml;nt&uuml; lay谋 qeyri-uy臒un olaraq altdan yatan struktur kompleksi &ouml;rt&uuml;r. Qurulu艧unda k&ouml;nd蓹l蓹n qalxmalarla ayr谋lan iki &ccedil;&ouml;k蓹klik var: Orta K&uuml;r (Yuxar谋 K&uuml;r &ccedil;&ouml;k蓹kliyi&nbsp;G&uuml;rc&uuml;stan Respublikas谋ndad谋r) v蓹 A艧a臒谋 K&uuml;r.</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">Ki&ccedil;ik Qafqazqaba臒谋 &ouml;n &ccedil;&ouml;k蓹kliyi Ki&ccedil;ik Qafqaz谋n Somxeti &mdash; A臒dam zonas谋na paralel, c蓹nub-艧蓹rq istiqam蓹td蓹 uzan谋r. O, Paleogenin fli艧 tipli v蓹 Neogen-Antropogenin molass formasiyal谋 &ccedil;&ouml;k&uuml;nt&uuml;l蓹rind蓹n t蓹艧kil olunmu艧dur; 艧imal-艧蓹rqd蓹 K&uuml;r d蓹r蓹si boyu Yevlaxad蓹k yax艧谋 izl蓹n蓹n K&uuml;ryar谋臒谋 il蓹, ondan 艧蓹rqd蓹 is蓹 B蓹rd蓹-Beyl蓹qan x蓹tti &uuml;zr蓹 ke&ccedil;蓹n fleksur 蓹yimi il蓹 h&uuml;dudlan谋r. &Ccedil;&ouml;k蓹kliyin q蓹rbind蓹 Ki&ccedil;ik Qafqazqaba臒谋 yar谋q il蓹 h&uuml;dudlanmas谋na baxmayaraq c蓹nub-q蓹rb s蓹rh蓹di girintili-&ccedil;谋x谋nt谋l谋d谋r.</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">Tal谋艧 q谋r谋l谋ql谋q sah蓹si Ki&ccedil;ik Qafqaz谋n m蓹rk蓹zi hiss蓹sinin bilavasit蓹 艧蓹rq davam谋n谋 t蓹艧kil edir. O, k&ouml;nd蓹l蓹n istiqam蓹td蓹 qalxm谋艧 Alpdan 蓹vv蓹lki b&uuml;n&ouml;vr蓹d蓹 yerl蓹艧ir; &Uuml;st Taba艧irin azqal谋nl谋ql谋 karbonat v蓹 Paleogen-Alt Eosenin fli艧 &ccedil;&ouml;k&uuml;nt&uuml;l蓹rind蓹n, Orta Eosen traxibazaltlar谋ndan v蓹 Oliqosen fli艧 &ccedil;&ouml;k&uuml;nt&uuml;l蓹rind蓹n t蓹艧kil olunmu艧dur. Sah蓹nin ki&ccedil;ik inruziv k&uuml;tl蓹l蓹ri Paleogend蓹 yerl蓹艧ir v蓹 q蓹l蓹vi bazalt, qabbro, diabaz-diorit v蓹 qabbro-monsonit-siyenit formasiyalara aid olub, yerl蓹艧diyi vulkanogen s&uuml;xurlarla birlikd蓹 vahid maqmatik kompleks 蓹m蓹l蓹 g蓹tirir.</span></span></p> <p style="text-align:justify"><span style="font-size:14px"><span style="font-family:arial,helvetica,sans-serif">Burada Astara v蓹 Burovar antiklionriumlar谋, Yard谋ml谋 v蓹 C蓹lilabad sinklinoriumlar谋, faylar, &uuml;st蓹g蓹lm蓹l蓹r v蓹 onlar谋 m&uuml;r蓹kk蓹bl蓹艧dir蓹n k&ouml;nd蓹l蓹n qalz谋m v蓹 &ccedil;&ouml;k蓹klikl蓹r ayr谋l谋r.</span></span></p> </article> </section> <footer> <div class="menubar footer-container" id="footer-load"></div> </footer> </div> <script src="/assets/110dab23/jquery.js"></script> <script src="https://cdnjs.cloudflare.com/ajax/libs/tiny-slider/2.8.5/min/tiny-slider.js"></script> <script src="/media/javascripts/script.js?v=280823"></script> </body> </html>

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