Qaab dhismeedka Tectonic Caraabaah Yurub East. The gargaarka of East Bannaankii Yurub

East Plain Yurub waa qayb ka mid ah madal Bariga Yurub. Tani waa qaybta hore iyo mid deggan, la suumanka koontoroolidda duubnaadaan. In madal bari fadhiyo Urals. Qaab dhismeedka Tectonic of East Bannaankii Yurub waa in koonfurta waxay xuduud la leh suunka Mediterranean duubnaadaan oo saxan Iskutees, kaas oo degan meel ka mid ah Pre-Caucasus iyo Crimea. oo soohdintu waxay la kordhiyay afka Danube ka, oo ay weheliso Black iyo Azov ee Badaha.

tectonics

Qaab dhismeedka tectonic Complex of East Bannaankii Yurub waxaa lagu bartay by saynisyahano badan. Khubarada arrimaha dibadda u wac Ruush (si la mid ah sida boosteejo ah). Qayb ka mid ah, iyada oo soohdintiinna koonfureedna waxay maraa gobolka Tsimlyansk kaydka. Waxaa jira a logu talagalay dhulka ee waaweyn - joojin yurubta bari Chief. Dhismaha madal deegaanka ay tani tahay mid aad u adag, sida juts gelin cufayo saxan Iskutees.

Maaddaama ay meesha dhismeedka wayn tectonic Bariga Yurub Caraabaah sinnayn. Seynisyahanno ku go'doonsan laba dibnaha waaweyn-gaashaan (Yukreeniyaan iyo Baltic) iyo sidoo kale dhowr goobood oo aasaas gogosha gacmeed oo qoto dheer. Waxay ka kooban yahay Archean, Proterozoic iyo si qoto dheer qaababka.

ceegaagta Archean

Heer-dhismeedka tectonic of East Bannaankii Yurub waa in aasaaska loo geysto degaanka ee Shield bari ee Karelia iyo Peninsula Kola ah. Waxaa la mid ah oo laga dheehan karo ka lakabka Archean in Konotop, Podolsky iyo Arrays Dnieper. Halkan uu ka wakiil yahay amphibolites, migmatites iyo gneisses. In dhagaxyada, kuwaas oo ay kooxahaasi badan oo quartzite ferruginous iyo graphite. Da'dooda - 3 milyan oo sano.

Tusaale kale oo daaha Archean - anticline Voronezh, halkaas oo aasaas waxaa la dhigay on the aan aad u qoto dheer. Waxay ka kooban tahay qaababka Kobenhagen iyo femic. dhagaxyada Kuwan waxaa lagu gartaa tiro badan oo loo calaanjin of Halabuurka acidic iyo aasaasiga ah, da'da taas oo ku saabsan 2.7 milyan oo sano.

Qaadista iyo korinta

Asal ahaan, Bariga Plain Yurub - cover boosteejo ah oo la duubnaadaan korsiiya ah Proterozoic, Paleozoic, Mesozoic iyo Zaman Cenozoic. bulukeeti aasaaska Ruush duwan yahay gargaarka sineyn ee aasaaskii saqafka. Its qaab-dhismeedka waxaa loo qaybiyaa afar qaybood subsidences hoose iyo uplifts. Waxay sidoo kale u beddelid kasta oo kale. Tani waa meesha Caspian of dagitaan, uplift aagga Sarmatian, meesha Baltic-Central Ruush ah dagitaan iyo uplift aagga bari.

Awoodda celceliska madal yahay 35 ilaa 40 km (awood badnaan go'an at anticlise Voronezh - 55 kiiloomitir meesha awgii lakabka basalt joogo). tirada ugu yar ee khuseeya syncline Caspian ah. Qaadayso lakabka basalt keentay in crustal khafiifiya aulacogene Pachelma.

isugu soo Caspian

da'da saxda ah ee East Bannaankii Yurub - 1.6-2.6 milyan oo sano (ugu da'da weyn ee goobaha ay ku yaalaan qaybta bari). By Arrays dheer-taagan waxaa ka mid ah Tatar, Caspian iyo Zhiguli-Pugachevsky. Waxay la wadaago kiiska protoplatformenny. soo diyaariyeen ugu weyn - Caspian. In Samara oo Saratov Trans-Volga Volga waxa ku jira ceelka. Waxay shaaca ka qaaday alumina sare gneisses Archean iyo schists.

isugu soo Caspian kharash ku wixii la goostay by height of East Bannaankii European on xuduudaha ay koonfur-bari, qaab-dhismeedka gaar ah oo kala duwan oo qoto dheer. In ay xarunta jiro lakabka dhagax adag ah, laakiin u kaca ku sugan basalt iyo highs cuf Aralsorskom Hobdinskom. Sawirka kale waa on duleedka safi. Waxaa jooga daaha thinned of dhagax adag.

syneclise Prikaspiyskaya ka mid ah domes badan oo cusbo. On galbeed iyo xagga woqooyi dhinacyadeeda waxaa jira unu qoto dheer (stage Volgograd, qarka Yulia Zhadovskaya Tokarevskaya flexure). Aasaaskii loo dhigi si qoto dheer ah 25 kiiloomitir. domes Salt waxaa ugu horumarsan ee degaanka Guryev. tirada ay noqon kartaa boqollaal kiilomitir oo laba jibbaaran. Waxay leeyihiin qaab saddex xagal, wareeg iyo elliptical xataa. The domes cusbo ugu weyn - Chelkarsky, Dossorsky, Inder, Makat, Eltonsky iyo sonkor-Lebyazhinsky.

Syncline iyo anticline

Moscow syneclise - ugu weyn ee madal Ruush. Noocan oo kale ah, oo ay ka qeyb dhexe ee East Bannaankii Yurub. Photo iyo cilmi Haseyeeshee ayaa muujinaya in ay ku laayeen waqooyiga waxaa jira laba qaadista (Soligalichskoe iyo Sukhonsky). Qaybta ugu badan ee syncline loo dhigi dhow Syktyvkar, kaas oo la ogan karo dhowr domes cusbo (qubbad Seregovskie), la dhisay oo cusbo Devonian. Salkeeda waa aulacogene Srednerussky lakabka ah baruurta ka buuxsamay.

Cunsur kale oo muhiim ah oo ah bannaanka tectonic - ka anticline Volga-Ural. Waxay ka kooban tahay a Niyadjabka weyn oo sarreeya. Anticline waxa lagu gartaa qaab adag. Its quruxsan ugu weyn - wareegga Tokmovsky in Mordovia. Sida laga soo xigtay anticlise baxa gobollada muhiimka ah biyo mareen - Volga ah. Wabiyaal kale ee waaweyn ee East Bannaankii Yurub (Don ah, Dnieper, Western Dvina) liita iyada ku aagga balliga iyo sifooyinka kale.

gargaarka

height Celceliska East Bannaankii Yurub waa 170 mitir. Heerka ugu sareeya waxaa laga soo qoray ee buurta Ural ee Tatarstan (479 mitir). Guud ahaan, dhul guriga kala duwan taas oo ku xidhan gobolka. Qaybta dhexe waxaa loo qaybiyaa dhowr dhulka talantaalli ah iyo uplands. The ugu horeysay oo ka mid ah waxa uu ku yaalaa dooxadii Oka, xagga woqooyi ka duwan Donetsk. Upland Tani. Inta lagu guda jiro glaciation Dnieper ah waxaa ku dednaa by sitoos ah. Tani waa caddaynta ku kayd sifo, oo ay ku jiraan moraine ku Dhiniciisa Midig, Oka, oo u dhow Serpukhov.

Urals waa buuraha Bugulmino-Belebei. Waxaa la buur ah oo ugu dhaceen sloping taagga. Waxay ka kooban yahay siltstone, nuuradda, dhoobo, marl iyo sandstone. Waxaa jira dad badan godad karst iyo godad. gargaarka Erosive dissected by Wabiyaal - addoommo ah, Volga ku Kama iyo Belaya. Hill saliidda hodanka ah (Romashkinskoye, Tuymazinskoe, Shkapovskoe). dalcadaha Gentle kaymaha ka nugul yihiin ku syrts top.

Volga Upland

On Dhiniciisa Midig, Volga bilaabmin Volga Upland. Waxaa kala ka Volgograd in Nizhny Novgorod, iyo xagga galbeed waa ku xiga si ay dooxada Tambov. Caraabaah Relief Bariga Yurub ee ka qeyb this sameeyay sabab u ah burburinta dhagaxa weyn, ka dib markii taas waxaa la sameeyey dhoobo, ciid, aan nuurad lahayn, marl iyo sibraar. All kayd kuwanu waa Paleocene, Jacka iyo Cretaceous.

More outcrop nuuradda Permian iyo Carboniferous qadiimiga ah iyo adag on the bangiyada of laab Samara ah. Waxaa ka mid kayd ah waa in sidoo kale muujiyo sandstones xoog leh. dhulka hoostiisa crystalline of Uplands Volga la yareeyo si qoto dheer ka weyn (oo ku saabsan 800 mitir).

The u dhaw in ay ku-Oka Don dooxada, dusha ka badan hoos. Volga dalcadaha yaacday ilaa iyo dissected by webiyada, iyo gullies badan. Taas darteed, waxaa la sameeyay dhul Patriots.

Total Sirt iyo bannaankaba Oka-Don

Total Sirt - qayb kale oo muhiim ah oo ka mid ah gargaarka, taas oo kala duwan ee East Bannaankii Yurub. Photos of gobolka this on soohdinta reer chernozem aagga Russia iyo Kazakhstan show, carradu Chestnut iyo carradu biyaha cusbada jirta ee watersheds iyo webiyada. Guud ahaan Syrt Zavolzhe ka bilaabantaa oo kordhiyay 500 kiiloomitir bariga. Waxaa inta badan ku yaal aagga u dhexeeya Greater oo yar Irgiz Irgiz, bari xiga si ay u Urals Southern.

Inta u dhaxaysa Privolzhskaya iyo Upland ku yaal Oka-Don dooxada. Its qayb waqooyiga waxaa sidoo kale loo yaqaan Meschera. oo soohdintu waxay waqooyi ee dhulka jooggiisu hooseeyo waa Oka. In koonfurta ee ay xuduud dabiici ah - Kalach Upland. qayb muhiim ah oo dalkii dooxada ahaa - Oka-Tsninsky usheeda dhexe. Waxaa kala dhex Morshansk, Kasimov iyo Gogol. In meelaha woqooyi ah ee Oka Don dooxada soo sameeyey kayd glacial, iyo xagga koonfureed waxaa saldhig u ah ciid.

Valdai iyo Northern Uvaly

weyn East Plain Yurub ayaa waxa uu ku yaalaa inta u dhaxaysa ee Atlantic iyo badaha Arctic. The maddiibadood oo webiyaasha in qulquli iyagii soo gashay, laga bilaabo on Hills Valdai ah. Its dhibic ugu sareeya - 346 mitir. Valdai waxa uu ku yaalaa Smolensk, Tver iyo gobollada Novgorod. Waxaa lagu gartaa moraine buur ah xigtaa-iyo gargaarka. Waxaa jira wax badan oo biyagaleenka ahuba iyo harooyinka (oo ay ku jiraan Lake Seliger iyo Verhnevolzhskie).

Qaybta waqooyi ee East Bannaankii Yurub - Northern Uvaly. Waxay mashquulin dhulka Jamhuuriyadda gobollada Komi, Kostroma, Kirov iyo Vologda. Oo ka kooban buuraha lahaa, si tartiib ah hoos u jihada a northerly ilaa ay ku dul dhanka ah White iyo Barents Badaha. Its height ugu badnaan - 293 mitir. Northern Uvaly - weysada lagu qaybsanyahay of Northern Dvina iyo Volga ah.

dooxada Badda Madow

In koonfur-galbeed ee East Bannaankii Yurub dhamaado Badda Madow dooxada, ee ku taalla soohdinta reer Ukraine iyo Moldova. On hal dhinac waxaa kumyadu by Delta Danube, oo ku kale - webiga Azov Kalminus. The dooxada Badda Madow ka mid ah neogenovyh iyo paleogenovyh Fat (dhoobo, ciid iyo nuuradda). Waxay hor istaagay gudboon iyo loess.

Dooxada dooxooyinka gudbay dhowr Wabiyaal: Dniester ah, bahal Koonfurta iyo Dnieper. bangiyada waa dhul uga yaacday ilaa iyo noqnoqda kala duwan. On xeebta estuaries badan (Dniester, Dnieper, iyo D. sidaas on.). Muuqaal kale oo la garan karo - tiro badan oo tufo ciid. In Black Sea dooxada muuqaalka steppe heysatay la madow cawlan iyo ciidda madow. Tani waa ka di'in hodan beeraha.