
intraplate vaikalyam

intraplate vaikalyam anedi bhoomi yokka crust yokka madata, vichchinnam ledhaa pravaham, vaati anchula vadda kakunda plaetla lopala. eee prakriya saadhaaranamgaa tibeton peethabhoomi (chitram 1) vanti mukhyamgaa balaheenamaina crust mariyu eguva montil unna praantaalalo jarugutundi. intraplate vaikalyam plate tectonic siddhaantaaniki maroka amsaanni testundi.
crustal vaikalyam prakriyalu.
plate tectonics siddhaantam prakaram bhoomi yokka lithosphere (crust mariyu eguva montil) drudamaina plaetlatoe tayaarai untundi, ivi osthenosphere (diguva montil) paina "theeluthuu" okadaanikokati saapekshamgaa kadulutaayi. plaetlu kadulutunnappudu, crust plate anchula venta pradhanamgaa vaikalyam chendutundi. kevalam plate anchula vadda matrame kakunda crust balaheenamgaa unna chota vaikalyam sambhavinchavacchani pariseelana dwara intraplate vaikalyam aaa vishayamlo bhinnamgaa untundi.
vaikalyam antey raalla madata, vichchinnam ledhaa pravaham. raallu pelusugaa unnaya ledhaa namyaga unnaya anae daanipai aadharapadi aneka rakaala crustal vaikalyalu unnaayi. eee lakshanaalanu nirnayinche amsaalu bhoomilo raallu anubhavinche konni ushnogratalu mariyu ottilla kaaranamgaa untaayi. anduvalla, ushnograta mariyu peedanam niyantrana vaikalya prakriyalu. saage silalu kudimpu ledhaa vistarana saktula kaaranamgaa vangi, madavutaayi, saagadeeyabadataayi ledhaa pravahistaayi. marovaipu pelusugaa unde raallu virigipotaayi. crust virige praantaanni falt antaaru. moodu pradhana rakaala lopaalu unnaih
saadhaarana lopaalu, riverse lopaalu ", mariyu strike slip (transform) lopaalu.
vividha rakaala plate anchula kaaranamgaa crust vaikalyam chendagala margalu ivi, avih
vibhina sarihaddulu, kalise sarihaddulu mariyu sarihaddulanu marchadam. 
eee moodu sarihaddulu ellappuduu sampuurnamgaa erpadavu mariyu idhi mishrama sarihadduku daariteestundi. mishrama sarihaddulu convergence thoo transform kalayika ledhaa divergence thoo transform kalayika kaavacchu.
intraplate vaikalyaaniki udaaharanalu.
asea.
madhya/thoorpu asea bahusha pedda ettuna intraplate vaikalyaaniki uttama udaaharana. tibeton peethabhoomi mariyu himalaya parvata shreni nirmaanam mariyu abhivruddhi sumaru 50 million samvatsaraala kritam senozoic yugamlo bharatiya phalakam eurasian falakaanni dheekonnappudu praarambhamaindi. eee gharshana kaaranamgaa lithosphere chaalaa chinnadigaa maarindi, idhi himalaya/tibet praantamloo crustal mandam mariyu adhika ottidini penchindi.
tibetloni aneka bhougolika pariseelanalu balaheenamaina crustal jonnu chuuputaayi mariyu madhya nundi diguva crust dravaalanu kaligi undi paakshikamgaa kariginchavacchani suuchistunnaayi. himalayan-tibet praantam peragadam praarambhinchadamtho, tibeton peethabhoomilo crust yokka parshwa velikiteeta kramamga dheekonadam mariyu crustal shorteningnu sardubaatu cheyadaaniki aadhipatya yantraamgaa maarindi. parshwa velikiteeta pradhanamgaa thoorpuku mariyu bharatadesam yokka maargam nundi bayataku jaarutondi. thoorpu tibet saampradayakamgaa vistruta vasati mandalamlo bhaagamgaa nirvachinchabadindi. thoorpu kadalikalo ekkuva bhaagam pradhana strike-slip lopaala kaaranamgaa undhi. tibetloni itara lopalatho paatu eee strike-slip lopaalanu ippatikee plate maarjinlo unnatlu ardham chesukovacchu. nijamaina intraplate vaikalyam mangolia ledhaa tian shaan parvataalu vanti praantaalalo uttaraana marinta dhooramlo sambhavistundi. eee praantaalu nijamaina intraplate vaikalyanni pradarsistaayi endukante plate anchuku vandala kilometres dhooramlo unna india/eurasia gharshana nundi crustal shorteningku anugunamgaa inca chaalaa faulting mariyu madatalu unnaayi.

