anticline - Meaning in Hindi

Meaning of anticline in Hindi

  • ऐन्टिक्लाइन

anticline Definition

  • a ridge-shaped fold of stratified rock in which the strata slope downward from the crest. ( स्तरीकृत चट्टान का एक रिज के आकार का तह जिसमें शिखा से नीचे की ओर ढलान होती है। )

anticline Example

  • In its hanging wall, however, a drag fold syncline and a rollover anticline developed. ( इसकी लटकती दीवार में, हालांकि, एक ड्रैग फोल्ड सिंकलाइन और एक रोलओवर एंटीक्लीन विकसित हुआ। )
  • The field evidence includes the presence of several longitudinal extensional folds such as a rollover anticline and drag folds that are related to normal faults in the area. ( क्षेत्र के सबूतों में कई अनुदैर्ध्य बहुआयामी सिलवटों की उपस्थिति शामिल है जैसे कि रोलओवर एंटीक्लीन और ड्रैग फोल्ड जो क्षेत्र में सामान्य दोष से संबंधित हैं। )
  • Present along the surface exposures of the anticline are rocks dating from Upper Cretaceous to Paleocene age. ( एंटीक्लीन की सतह के साथ मौजूद हैं ऊपरी क्रेटेशियस से पेलियोसीन उम्र तक की चट्टानें हैं। )
  • From the maps presented in Figure 2, it is apparent that the well tested the crest of an anticline that formed during the Cenozoic. ( चित्र 2 में प्रस्तुत मानचित्रों से, यह स्पष्ट है कि अच्छी तरह से एक एंटीक्लीन के शिखा का परीक्षण किया गया था जो सेनोजेनिक के दौरान गठित हुआ था। )
  • This mechanical failure results in a topographic valley along the crest of the anticline . ( इस यांत्रिक विफलता के परिणामस्वरूप एंटीक्लाइन की शिखा के साथ एक स्थलाकृतिक घाटी बन जाती है। )
  • In this locality, the top 20 m of the Asmari Limestone exhibits palaeo-weathering along joints suggesting subaerial exposure of the Asmari near the crest of an anticline . ( इस इलाके में, अश्मरी लिमस्टोन के शीर्ष 20 मीटर में जोड़ों के साथ पैलियो-अपक्षय का प्रदर्शन होता है, जो एक पुरावशेष के शिखर के पास अस्मरी के उप-प्रदर्शन का सुझाव देता है। )
  • However, as the thrust sheets grow, the outer area of their anticlinal crest is extended. ( हालांकि, जैसे-जैसे जोरदार चादरें बढ़ती हैं, उनके एंटीकाइनल शिखा के बाहरी क्षेत्र को बढ़ाया जाता है। )
  • These fault-parallel footwall anticlines are best developed along fault segments 3 and 4, although there are also examples of fault-parallel folding in the footwall of fault segments 1 and 2. ( ये दोष-समानांतर फुटवॉल एंटिकलाइन फॉल्ट सेगमेंट 3 और 4 के साथ सबसे अच्छे रूप में विकसित होते हैं, हालांकि फॉल्ट सेगमेंट 1 और 2 के फॉल्ट-समानांतर फोल्डिंग के उदाहरण भी हैं। )
  • These metamorphic and plutonic igneous rocks form the uplifted core of the broadly anticlinal Owl Creek Mountains, a mountain range that formed during the Late Cretaceous. ( ये मेटामॉर्फिक और प्लूटोनिक आग्नेय चट्टानें मोटे तौर पर एंटीक्लिनल उल्लू क्रीक पर्वत के उत्थान कोर का निर्माण करती हैं, जो एक पर्वत श्रृंखला है जो लेट क्रेटेशियस के दौरान बनाई गई थी। )
  • Watterson et al. explained that this situation can arise due to local extension and thinning associated with anticlinal folding of the beds overlying the ridges in the low velocity layer. ( Watterson एट अल। समझाया कि यह स्थिति स्थानीय विस्तार और कम वेग परत में लकीरें खींचने वाले बिस्तरों के एंटीकाइनल तह से जुड़े पतले होने के कारण उत्पन्न हो सकती है। )
  • Although it is counterintuitive for a graben to overlie a ridge, it has long been recognized that graben can result from local extension and thinning in the anticlinal domains that overlie linear ridges. ( यद्यपि यह एक रिज को ओवरलेन करने के लिए एक अति महत्वपूर्ण है, लेकिन यह लंबे समय से माना जाता है कि ग्रैबिन स्थानीय विस्तार और एंटीक्लिनल डोमेन में थिनिंग के परिणामस्वरूप परिणाम ला सकता है जो रैखिक लकीरें खींचता है। )
  • The salt continued moving along lines of least resistance and began to push upward, bowing up the overlying sedimentary rocks to form the classic elongated anticlinal structure. ( नमक कम से कम प्रतिरोध की रेखाओं के साथ आगे बढ़ता रहा और क्लासिक लम्बी एंटीकाइनल संरचना बनाने के लिए अतिव्यापी तलछटी चट्टानों को झुकाते हुए ऊपर की ओर बढ़ने लगा। )

More Sentence

  • The displacement of the thrust sheet produces two anticlines and a syncline.
  • The expelled hydrothermal fluids were trapped in cap-rock situations inside anticlinal zones, such as the major lithological contrast between siliceous limestones and black shales at the flanks of the Arnsberg anticline.
  • These subterranean muds are being uplifted into steeply dipping, anticlinal structures cored by strike-slip faulting.
  • Large-scale geological structures including anticlines , synclines, thrusts and faults formed during the Caledonian Orogeny typically trend in a SW-NE direction.
  • The Zagros Simply Folded Zone can be distinguished from the rest of the orogen by NW-SE-trending parallel folds and thrust-cored anticlines which verge to the SW in a 6-12 km thick cover sequence.
  • These elongate anticlinal domes have gentle to moderate dips on their flanks, and are cut by several thrust faults that may be linked to a deeper system.
  • The rocks are on the west flank of the Monument uplift, a 60-mile-long north-trending anticlinal structure.
  • Its topography, represented by the alleged anticlines and synclines of Rosenkrantz, is instead an expression of the original sea-floor topography.
  • This mountain illustrates both anticlinal and synclinal folding and the way in which the two different fold types react to weathering and erosion.
  • Secondly, along-strike displacement minima, fault jogs and anticlinal intrabasin highs often form at, and represent the location of, palacosegment boundaries and subsequent zones of segment linkage.
  • The precise form of the anticlinal folds at the base of the overburden layer is uncertain because of both limited seismic resolution and complexities due to the near convergence of conjugate-fault pairs.
  • It has been previously reported that because of extension of the outer arc of such anticlines , graben form above their crests.
  • The origin of this circular anticlinal structure has been the subject of a longstanding debate.
  • Strain differences between anticlinal and synclinal domains of concentric fold stacks require discontinuities between the two types of domain to maintain overall strain compatibility.
  • It is possible that faulting along the crests of deep-seated anticlines provide the conduit for mobile muds to migrate through to the seafloor surface.
  • Tectonic movement locally folded and uplifted the Pabdeh Formation exposing it to erosion along the crests of anticlines before this unconformity was buried beneath the Asmari Limestone.
  • Following the intrusion of basic dykes in the late Palacocene, the whole of the post-Zechstein succession was gently folded into a series of major synclines and anticlines .
  • However, with progressive deformation, markers above anticlinal crests were extended in the shortening direction.

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