ib qho loj thiab complex txheej txheej txheej ntawm cov quav hauv lub strata ntawm lub ntiaj teb crust uas tshwm sim nyob rau hauv geosynclines vim loj thiab protracted uplifts nyob rau hauv lub ntiaj teb crustuas yog nrog los ntawm folding txheej txheem thiab tus yam ntxwv los ntawm ib tug dav uplift nyob rau hauv qhov chaw.
Anticlinorium yog dab tsi hauv thaj chaw?
Ib qho tshuaj tiv thaiv kab mob yog tus kab mob loj heev uas cov quav me me yog superimposed, thiab ib qho synclinorium yog ib qho loj syncline uas me me quav yog superimposed. Lub symmetrical quav yog ib qho uas lub dav hlau axial yog ntsug.
Dab tsi ua rau muaj kev tiv thaiv kab mob?
Sedimentation and Oil/Gas Formation
Anticline is a structural trap formed by the folding of rock strata into an arch-like shape. Cov txheej pob zeb nyob rau hauv ib qho cuab yeej anticlinal yog thawj zaug muab tso rau hauv kab rov tav thiab tom qab ntawd lub ntiaj teb txav tau ua rau nws fold rau hauv ib qho zoo li arch-zoo li hu ua anticline.
Yuav ua li cas thiaj rov tsim tau?
Nyob rau hauv quav. Ib qho quav rov qab muaj ib qho tseem ceeb kab rov tav axial dav hlau. Thaum ob txhais ceg ntawm ib lub quav yog qhov tseem ceeb sib npaug rau ib leeg thiab yog li kwv yees li ntawm qhov sib npaug mus rau lub dav hlau axial, lub quav yog hu ua isoclinal.
daim ntawv syncline li cas?
Synclines yog tsim thaum daim hlau tectonic txav mus rau ib leeg, compressing lub crust thiab yuam nws upward.