Note on the Liangshanophyllum,a new Subgenus of Waagenophyllum from Permian of China

The material of this short paper includes four species, one is a new form of Waagenophyllum, and the three others belong to a new subgenus named Liangshanophyllum. The specimens of the latter were collected by Y. H. Lu in 1942 from Liangshan, S Shensi, in a grayish black massive limestone, which is considered as the upper-most part of the Permian limestone at that region wish very abundant fossil corals of fasciculate cylindrical form. The new species of Waagenophyllum was collected in     

对于进行地质普查、矿区找矿和勘探工作的几点基本要求

在这个报告中我准备讲一下苏联对于进行地质普查、矿区找矿和勘探工作方面的几点基本要求和工作方法上的一些原则。在谈到本题从前,我想简单地谈谈保证地质调查工作能够顺利进行的一些一般的原则。     

L''■GE DU MARBRE DE FANG CHAN ET SA TENEUR EN MAGNESIE

Le beau marbre qui entre dans une si grande proportion dans la construction des palais et des monuments a Peking vient d'une region situee a 60 kilometres environ (a vol d'oiseau) au sud-ouest de la Capitable. C'est une partie du plateau qui borde immediatement la plaine alluviable qu'on     

A 2D finite volume model for bebris flow and its application to events occurred in the Eastern Pyrenees

FLATModel is a 2D finite volume code that contains several original approaches to improve debris-flow simulation. Firstly, FLATModel incorporates a ＂stop-and-go＂ technique in each cell to allow continuous collapses and remobilizations of the debris-flow mass. Secondly, flow velocity and consequently yield stress is directly associated with the type of rheology to improve boundary accuracy. Thirdly, a simple approach for entrainment is also included in the model to analyse the effect of basal erosion of debris flows. FLATMODEL was tested at several events that occurred in the Eastern Pyrenees and simulation results indicated that the model can represent rather well the different characteristics observed in the field.     

ON LOPINITE,A NEW TYPE OF COAL IN CHINA

To the east of Nanchang,the capital of Kiangsi Province,there cropsout a continuous belt of Permian coal series~1 trending approximately in thedirection from N.E.to S.W.Broadly speaking,this coal belt forms a synclinal     

О ПРЕДГОРНЫХ ОТЛОЖЕНИЯХ ЦАЙДАМА И ОТНОВНЫХ ЧЕРТАХ ЕГО РАЗВИТИЯ В ЧЕТВЕРТИЧНОЕ ВРЕМЯ

玖a众八aMeKa只K叮几oBHHa,oKpy水eHHa只roPHHMH eHeTeMaMH HaHb一山aH只,A几T曰H-Tara H KyHb一几yH只,no eBoeMy eTpoeHH幻只B几分eTe分THnHqH曰M nPe八eTaBHTe几eM Me米ro-PHHx Bna及HH玖eHTPa几bHo仑A3HH. O6mHPH班e reo卫orHqeeKHe Hee几e八oBaHH只B玖a益八aMe 6H几H HaqaTH ePaBHHTe卫bHoHe及aBHo一e 1955 ro八a B eB只3H e PasBe八Ko仑He中TeHoeHHx TPeTHqH曰x oT几。水eHH众BHn邸H分IO坦“x Bna八HHy.flo3ToMy reMorH只3Toro HHTepeeHoro pa直oHaB卫盯epaTypeocBe坦eHa noKae…     

On some Psilophyton-like Remains from the Tiaomachien Series in Central Hunan Senes Centra Hunan

It had long been my wish for an opportunity to collect more MiddleDevonian plants in the Tiaomachien series in central Hunan.InDecember 1936,I was able to realize my plans.I was fortunate enough     

AN UPPER PLIOCENE FLORULE FROM THE SANMENIAN SERIES OF SHANSI PROVINCE

The recent discovery of fossil plants in association with fresh-watermollusca,at the type locality of the Sanmenian series at Sanmen Rapids,addsa brief though important chapter to our gradually increasing knowledge of the     

Fossil Vertebrates from Kuangyuan, N. Szechuan, China

正 During the late spring of 1941, Messrs. M. N. Bien, T. H. Mi and the present writer were fortunate enough to discover several localities of vertebrate fossils. The geological condition will be reported in another paper' and need not be repeated there. Most of the fossils were derived from the hill     

NOTES ON THE GEOLOGY OF GREAT KHINGAN

In August 1933,I made geological investigations in the vicinity ofBarim station of Chinese Eastern Railway.This area was explored byDr.E.Ahnert in 1901~1,but my explorations were more in detail; I madegeological survey in the scale 1:10,000.All petrological determinations were