Results 121 to 130 of about 674 (167)

Genome-Wide Analysis and Expression Profiles of Auxin Response Factors in Ginger (<i>Zingiber officinale</i> Roscoe). [PDF]

Int J Mol Sci
Tong Y, Xu S, Shi J, He Y, Li HL, Yu T, Zhang S, Xing HT.   +7 more
europepmc   +1 more source

Anisotropic crack evolution and fractal failure mechanism of Lushan shale under compression: insights from acoustic emission. [PDF]

Sci Rep
Huang H, Zhou Y, Zhang Y, Wang C, Bi J.
europepmc   +1 more source

Clay minerals evidences for cold-warm fluctuations in the Early Silurian. [PDF]

PLoS One
Zhang Z, Zhang J, Wei H, Li H, Guo Y, Zeng C.   +5 more
europepmc   +1 more source

Differential sedimentary evolution of typical aulacogens of Meso-Neoproterozoic in North China craton. [PDF]

Sci Rep
Tan C, Lyu Q, Wang T, Li Q, Jiang H, Yan X.   +5 more
europepmc   +1 more source

FuseLinker: Leveraging LLM's pre-trained text embeddings and domain knowledge to enhance GNN-based link prediction on biomedical knowledge graphs. [PDF]

J Biomed Inform
Xiao Y, Zhang S, Zhou H, Li M, Yang H, Zhang R.   +5 more
europepmc   +1 more source

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On the upper Precambrian (Sinian Suberathem) in China

Precambrian Research, 1981
Abstract This paper gives a general outline of the Upper Precambrian (Sinian Suberathem) in China, including its geographic distribution, development, stratigraphic sequence and classification. The Sinian Suberathem, with a time range of 1950-615 Ma, constitutes the greater part of the Proterozoic.
Chen Jinbiao, Zhang Huimin, Xing Yusheng, Ma Guogan   +3 more
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Sinian glacial deposits in Xinjiang, Northwest China

Precambrian Research, 1985
Abstract Three levels of Sinian glaciogenic deposits are widespread in Xinjiang in northwestern China. Two of these are assigned to the lower Sinian and one to the upper Sinian. There is also some evidence for an older, fourth glacial episode. Continental, transitional and marine glacial deposits have been recognised; within these depositional ...
null Gao Zhenjia, null Qian Jianxin
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Geochemical Characteristics of Sinian Manganese Deposits in China

Acta Geologica Sinica, 2000
Abstract  Sinian is one of the main periods of the formation of manganese deposits in China. Sinian manganese deposits are mainly hosted in carbon‐rich black shale and siliceous shale formed during the Sinian interglacial period. The composition of manganese ore is simple. The main ore mineral is manganiferous carbonates.
ZHU Kaijun, YAO Guolong
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Integrated Ediacaran (Sinian) chronostratigraphy of South China

Palaeogeography, Palaeoclimatology, Palaeoecology, 2007
Abstract The Ediacaran Period was a critical time in the history of life and Earth. Understanding the complex interactions between geological and biological events during this interval requires high-resolution chronostratigraphy. Thanks to its uniquely favorable palaeogeographic setting, South China is an ideal region for constructing a framework for
Maoyan Zhu, Junming Zhang, Aihua Yang
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How Ibn Sinian Is Suhrawardi's Theory of Knowledge?

Philosophy East and West, 2003
It is demonstrated here that despite apparent differences and their adherence to two different schools of thought, Suhrawardi's epistemology is essentially Ibn Sinian, and even his theory of "knowledge by Presence" ('ilm al-huduri), which is considered to be uniquely his, is at least inspired by Ibn Sina.
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