Pore Structure Alteration Characteristics of Different Mineralogical Composition Shale during Shale-Fracturing Fluid Physical-Chemical Interactions by Zepeng Sun, Yongli Wang, Zhifu Wei, Yue Ni, Baoxiang Wu, Jing Li, Wenhua Fan, Gailing Wang, Yunxiao Li

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Isotopic Composition of Abiogenic Gas Produced in Closed-System Fischer-Tropsch Synthesis: Implications for the Origins of the Deep Songliao Basin Gases in China by Zhifu Wei, Yongli Wang, Gen Wang, Xueyun Ma, Wei He, Ting Zhang, Xiaoli Yu, Yan-Rong Zou

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Middle to Late Jurassic pelagites and gravity mass flow deposits of a displaced Neotethyan margin: Microfacies and biostratigraphical studies in Northeast Hungary by Haas János, Fodor László, Đerić Nevenka, Szives Ottilia, Ozsvárt Péter, Fialowski Melinda, Kövér Szilvia

“…This area represents the continuation of the Inner Dinaric nappesystem, and was displaced along the Mid‐Hungarian Shear Zone during the Late Oligocene to Early Miocene. The pre‐Cenozoic basement of the area is characterised by three juxtaposed units: the lowermost Recsk Succession, the Tarna Olistostrome and the topmost Darnóhegy Mélange nappe. …”
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The ground beneath our feet: A critical reflection on 135 years of landscape evolution models for southern Africa by Rivoningo Khosa, Vela Mbele, Kelly Kirsten, Robyn Pickering

“…He argues that this region of southern Africa is dry today and has been for much of the Cenozoic. This notion of long-term aridity and stability has dominated perspectives on southern African landscape evolution. …”
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Evaluation method and application for in-situ stress in No. 8+9 coal seam, southern Shenfu block, northeastern margin of Ordos Basin by Jiawei WU, Wei TANG, Yanhe ZHU, Cunwu WANG, Yongjing TIAN, Jingyu ZI, Jianghao YANG, Xian SHI

“…In the eastern part of the study area, the NNE-oriented maximum horizontal principal stress was sequentially evolved from the SN-oriented compression during the Meso-Cenozoic Indosinian stage, the NNW-oriented compression during the Yanshanian stage, and the NNE-oriented compression during the Himalayan stage. …”
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Upper Oligocene to Pleistocene planktonic foraminifera stratigraphy at North Atlantic DSDP Site 407, Reykjanes Ridge: diversity trends and biozonation using modern Neogene taxonomi... by T. M. Weitkamp, T. M. Weitkamp, M. J. Razmjooei, M. J. Razmjooei, P. N. Pearson, H. K. Coxall, H. K. Coxall

“…<p>Deep Sea Drilling Project (DSDP) Site 407, located near the Reykjanes Ridge (southwest of Iceland) offers a rare and extensive record of Late Cenozoic planktonic foraminifera evolution spanning the Neogene and Quaternary periods. …”
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Temporal and spatial heterogeneity of the Ailaoshan–Song Ma–Song Chay ophiolitic mélange, and its significance on the evolution of Paleo-Tethys by Lin, Wei, Liu, Fei, Wang, Yin, Meng, Lingtong, Faure, Michel, Chu, Yang, Nguyen, Vuong Van, Wu, Qinying, Wei, Wei, Thu, Hoai Luong Thi, Vu, Tich Van

“…The strike-perpendicular heterogeneity characterises the geometry of M1, M2, and M3 units and is attributed to a Cenozoic positive-flower structure of the Red River Fault showing sinistral strike-slip tectonic event with SW-ward thrusting. …”
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Petrology of Oligocene Lalehzar igneous rocks in the southeast of Saveh-Naein-Jiroft magmatic belt by Fatemeh Sepidbar, Bahareh Borouzi Niyat

“…Magmatism in the Saveh-Naein-Jiroft magmatic belt initiated in the late Paleocene, followed into the late Cenozoic, with a magmatic flare up in the Middle Eocene (Verdel et al., 2011). …”
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Petrogenetic evidences in geodynamics and placement of Nordoz intrusive masses in Alborz-Azerbaijan structural zone by Shahryar Mahmoudi, Shiva Lavi, Shohreh Hassanpour, Amir Ali Tabakh Shabani, Mehran Yegane Far

“…As the central portion of the Alpine-Himalayan orogenic belt, this region has experienced a number of geologic events as a consequence of the closure of the branches of the Neotethys Ocean (Stampfli et al., 1991). Cenozoic igneous rocks are pervasive in the Iran-Turkey region (Dilek et al., 2010). …”
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Whole-rock geochemistry and crystal chemistry of apatite at intrusive suites of the Qeynarjeh-Angouran district (west of Zanjan): an approach to the identification of skarn-causati... by Afsoon Dastour, Ebrahim Tale Fazel, Ashraf Torkian

“…The Takab-Angouran belt in the northwest of Iran hosts numerous mineral deposits from Neoproterozoic to Cenozoic, some world-class deposits (e.g., Angouran zinc and Zarshoran gold deposits) have been formed in this area. …”
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