晚白堊紀 的英文怎麼說

中文拼音 [wǎnbáiè]
晚白堊紀 英文
  • : 名詞1 (晚上) evening; night 2 (姓氏) a surname Ⅱ形容詞1 (時間靠後的; 遲) far on in time; la...
  • : Ⅰ形容詞1 (似雪的顏色) white 2 (清楚; 明白; 弄明白) clear 3 (空的; 沒加他物的) pure; clear; ...
  • : Ⅰ名詞(白堊; 白土) chalkⅡ動詞[書面語] (用白堊塗飾) cover with chalk; chalk
  • : 紀名詞(姓氏) a surname
  • 白堊紀 : chalk
  1. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

  2. Only in the tropics were numerous late cretaceous groups extinguished during peaks in their evolution.

  3. The hanging wall of sag extended in southeast direction, with the tulage fault being the boundary fault. yinggete - bagemaode metamorphic core complex developed adjacent to northwest of chagan sag, which evolved from late jurassic to cretaceous with three - layer construction style. the kinematics mechanism of metamorphic core complex and chagan sag is a simple shear model, chagan sag extended and faulted as the metamorphic core complex rised

  4. We have concluded that the structural movement of the area can be divided into three stages : the stretching stage from simian to early ordovician, the extrusion and rising stage from middle and late ordovician to jurassic and stable depressed stage of foreland basin slope from cretaceous to neozoic

  5. The study results can be summerized as following aspects : ( 1 ) the basic settling curve of this basin was broken - line shape of seven sections in which upper jurassic, lower cretaceous, eocene, oligocene and neogene corresponded with the decline ones representing five episodic clear subsidences of this basin, late cretaceous to paleocene and early miocene corresponded with the rising ones reflecting the uplift and denudation of this basin. ( 2 ) the subsidence of this basin migrated from the east to the west, from mesozoic to cenozoic

    研究表明: ( 1 )北黃海盆地的基本沉降曲線型式為7段折線狀,其中侏羅世、早世、始新世、漸新世、新近為曲線下降段,代表盆地5幕較明顯的沉降;世古新世以及中新世早期為曲線上升段,反映盆地的抬升剝蝕。
  6. Based on the analyses of structural features, volcanic activities, sequence construction and so on, it is believed that liaohe basin has experienced the period of dextral transtensional stress field in late jurassic - early cretaceous, middle and late paleocene, late eocene, miocene, and also the period of sinistral compresso - shear stress field in late cretaceous, early paleocene, early and middle eocene, oligocene, pliocene

  7. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演化史綜合方法,確認焉耆盆地侏羅系油氣藏具有三期成藏的特點,第一期發生在侏羅期,是盆地的主要成藏期,第二期為侏羅末至的油氣藏破壞、調整和再分配期,第三期發生在第三,是盆地的次要成藏期。
  8. The basin tectonic model : it is intermont basin during late jurassic to early cretaceous, developed into faulted - lacustrine basin in eogene, and evolved into depression in neogene and quaternary

  9. Through studying the stratigraphic framework of tectonic sequence, the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes

  10. Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward, which evolved from late jurassic to cretaceous. the extensional simple shear model of the chagan fault depression is established. the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure

  11. China sturgeon fish are produce in liaoxi china. they were formfd in remote antiouity of 150 million years ago

    鱘魚化石產于中國遼西,形成於侏羅- - -早,距近已有一億五千萬年。
  12. During my master " degree investigation, i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts, the eastern yanshan, and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution, volcanism and tectonism. then i summarized the mesozoic basin development and the coupling characters of basin and mountain. the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic, the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous

  13. Fish fossils are produced in china liao xi, they wear ed in remote antiqutty of 140. millionyears ago

    遼西古狼鰭魚化石標本- -產于中國遼西,形成於侏羅- -早,距今已有一億四千萬年。
  14. These rock formations were formed about 100 million years ago, and are a clear demonstration of the impact of water erosion

  15. And the hydrocarbon - generating is mainly from late cretaceous to tertiary, while traps formed mainly from late cretaceous to tertiary, prior to the hydrocarbon migration or simultaneously, with a fine coordination on the duration

  16. During this evolution, seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin, the arsuo tectonic melange zone, the taricuo - wenbu yenshan magmatic arc belt, the cuoqin - bangduo late paleozoic composite back - arc basin, the jiangrang - geerdi faulted uplift, the gangdise - chazi himalayan magmatic arc belt, and the xigaze - anba fore - arc basin. these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems. mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision

  17. It is a late cretaceous to tertiary basin located on the eastern part of the continental shelf of the east china sea ; it occupies an area of 59, 000 km2

    西湖凹陷是第三盆地,位於中國東海大陸架的東部,面積590000km2 ,處于緯度124030 '與127000 '之間,經度28030 '與31000 '之間。
  18. The extensional activities of hefei basin occurred in the period between late cretaceous and paleogene. as a result, the extensional normal faults were took place along the pre - existing nearly ew faults and the tan - lu fault zone. the deposition of half - graben was formed

  19. The evolution of the jurassic petroleum system can be divided into three stages : the forming stage in the late jurassic, the adjusting - destroying stages in cretaceous, and the activating - reconstructing stage in tertiary

  20. Through the analysis of subsidence history in the north of western ordos basin, as a result of the terranes northward accretion and the successive collision of the baykala block in the middle triassic, the qiangtang block in the late triassic, the lhasa block in the middle jurassic, the gangdese block in the cretaceous and the subduction of izanagi plate in yanshanian period, the studied region became a intracontinental foreland basin from late triassic to cretaceous