... Province, China (46°26 35.5 , 131°52 25.9 with an overall length of 79.7 m (Fig. 3A). The Heitai Formation unconformity overlies 541 484 Ma granite and is covered unconformably by Quaternary sediments. The lower section is composed of a medium- to coarse-grained sandstone neritic deposit, mainly land-shelf...

... of the landslides in Heitai terrace, China . Engineering Geology , 236 , 97 – 110 , doi: 10.1016/j.enggeo.2017.09.016 10.1016/j.enggeo.2017.09.016 Peng , J.B. , Zhang , F.Y. and Wang , G.H. 2017 . Rapid loess flow slides in Heifangtai terrace, Gansu, China . Quarterly Journal...

...HONG-HE XU; YI WANG Abstract Morphology of the leaves of stem compressions originally attributed to Protolepidodendron scharyanum from the Middle Devonian of North Xinjiang, China is reinvestigated. The leaf is three-dimensional, consisting of one central abaxial segment and four lateral adaxial...

..., Heilongjiang Province, NE China, indicating a Middle Devonian age (Ouyang, 1984 ), although no taxa at the species level are shared by the Heitai assemblage and that of the PM90 succession. Another line of evidence for the age of the flora is based upon 206 Pb/ 238 U ages of detrital zircons from bed-13...

...Jianbing Peng; Fanyu Zhang; Gonghui Wang * Correspondence: [email protected] © 2017 The Author(s) 2017 The authors would like to apologize for the following error in Figure 1b , on page 106. The two sites of Heitai and Fangtai were mistakenly labelled as each other...