冬眠
发表于 2025-4-1 02:16:27
Ch. Chinnappa,Pauline Sabina Kavali,A. Rajanikanth,Mercedes di Pasquo,M. E. C. Bernardes-de-Oliveirader article on the same subject, written by one of us (H.A.B.) about 25 years ago for the Geiger-Scheel .Handbuch der Physik.. To the article written last year we have added some Addenda and Errata. These Addenda and Errata refer back to some of the 79 sections of the main text and contain some misprint corre978-0-306-20022-9978-1-4613-4104-8
Adrenal-Glands
发表于 2025-4-1 06:42:27
http://reply.papertrans.cn/64/6311/631067/631067_62.png
integrated
发表于 2025-4-1 10:19:20
R. Nagendra,A. Nallapa Reddyder article on the same subject, written by one of us (H.A.B.) about 25 years ago for the Geiger-Scheel .Handbuch der Physik.. To the article written last year we have added some Addenda and Errata. These Addenda and Errata refer back to some of the 79 sections of the main text and contain some misprint corre978-0-306-20022-9978-1-4613-4104-8
低位的人或事
发表于 2025-4-1 17:02:37
A Review of Stratigraphy, Depositional Setting and Paleoclimate of the Mesozoic Basins of India,nates, along with profuse terrestrial fauna and flora. The Early Jurassic sediments of Barmer and Jaisalmer were essentially deposited in fluvio-lacustrine environment under humid climatic condition. With the advent of Middle Jurassic, limestone started depositing in the Mesozoic basins. The Middle
惊惶
发表于 2025-4-1 19:52:33
Cretaceous Deposits of India: A Review,t, west coast, and offshore basins in response to the rise in RSL during Albian, Turonian and Campanian. A Late Cretaceous transgression in central India came from the west. The maximum fossil foraminifer diversity was in the late Cenomanian/earliest Turonian and this time-interval is corresponding
就职
发表于 2025-4-2 01:55:15
Radiation of Flora in the Early Triassic Succeeding the End Permian Crisis: Evidences from the Gondorthern part of Tatapani-Ramkola Coalfield. The macrofloral assemblage of the Raniganj Formation (late Permian) from the base of the outcrop is represented by . sp. and . sp., whereas the overlying Panchet Formation (early Triassic) yielded a moderately preserved macrofloral assemblage represented b