Mesozoic and Cenozoic accretionary orogenic processes in Borneo and their mechanisms-Reference-Cited by-同舟云学术

Mesozoic and Cenozoic accretionary orogenic processes in Borneo and their mechanisms

Author:

Wang P. C.¹²,Li S. Z.¹²,Guo L. L.¹²,Jiang S. H.¹²,Somerville I. D.³,Zhao S. J.¹²,Zhu B. D.⁴,Chen J.⁴,Dai L. M.¹²,Suo Y. H.¹²,Han B.⁴

Affiliation:

1. College of Marine Geosciences; Ocean University of China; Qingdao Shandong China

2. Key Lab of Submarine Geosciences and Exploration Techniques, Ministry of Education; Qingdao Shandong China

3. UCD School of Earth Sciences; University College Dublin; Dublin Ireland

4. Guangzhou Marine Geological Survey (GMGS); Guangzhou China

Funder

NSFC

National Programme on Global Change and Air-;Sea Interaction, SOA

Aoshan Elite Scientist Plan

Taishan Scholar Program

Publisher

Wiley

Subject

Geology

Reference106 articles.

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2. Lower Cretaceous from the Chert-Spilite Formation, Kudat, Sabah Warta Geological;Basir;Geological Society of Malaysia Newsletter,1985

3. Barremian radiolaria from the Chert-Spilite Formation, Kudat, Sabah;Basir;Sains Malaysiana,1988

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