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<jats:p>The source of oil and gas in the Tarim Basin's platform has always been controversial. The Lower Cambrian Yurtusi Formation and the Xidashan Formation–Xishanbulak Formation argillaceous source rocks are an important set of oil source series in the basin. Based on the principle of conservation of matter, this paper calculates the hydrocarbon expulsion amount of the source rock. Using a phase state hydrocarbon expulsion amount characterization model, the paper reconstructs the evolution process of the hydrocarbon expulsion phase state of the source rock. According to the characterization model of hydrocarbon expulsion dynamics, the relative contribution of each force to hydrocarbon expulsion is evaluated. The hydrocarbon expulsion geologic model of argillaceous source rocks in the Lower Cambrian in the Tarim Basin is established. The results show that this set of source rocks can serve the main source rocks in the basin. The hydrocarbon expulsion of the Lower Cambrian argillaceous source rocks in the Tarim Basin can be divided into three stages. In the first stage, the hydrocarbon expulsion phase is dominated by the water‐soluble and diffusion phases. The conversion of clay minerals into dehydration and diffusion forces is the main driving force for the hydrocarbon expulsion. In the second stage, the oil and gas expulsion present the characteristics of multiphase and multidynamic coexistence. In the third stage, the phase state of oil and gas expulsion is mainly free phase. The capillary force difference and the thermal expansion force of the fluid rock are the main driving forces for oil and gas expulsion. The research results of this paper can deepen the understanding of the hydrocarbon expulsion mechanism of the set of source rocks, and then guide oil and gas exploration.</jats:p>

<jats:p><jats:bold>RETRACTION</jats:bold>: Y. Li, “Joint impact of technological innovation and energy consumption on natural resource management: Evidence from the Asian developing region,” <jats:italic>Geological Journal</jats:italic> 58, no. 9 (2023): 3385–3400, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="https://doi.org/10.1002/gj.4811">https://doi.org/10.1002/gj.4811</jats:ext-link>.</jats:p><jats:p>The above article, published online on 27 July 2023 in Wiley Online Library (<jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="http://wileyonlinelibrary.com">wileyonlinelibrary.com</jats:ext-link>), has been retracted by agreement between the journal's Editors in Chief, Ian D. Somerville and Yunpeng Dong; and John Wiley &amp; Sons Ltd. The retraction has been agreed following concerns raised by a third party. Further investigation by the publisher has found manipulation of the peer review process. The retraction is warranted due to the compromised integrity of the article's peer review.</jats:p>

<jats:p><jats:bold>RETRACTION</jats:bold>: M. Tao, B. Zhang, G.B.A. Kizi, “Measuring the management of natural resources and regional sustainable development: Mediating role of green finance in China,” <jats:italic>Geological Journal</jats:italic> 58, no. 9 (2023): 3278–3287, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="https://doi.org/10.1002/gj.4820">https://doi.org/10.1002/gj.4820</jats:ext-link>.</jats:p><jats:p>The above article, published online on 13 July 2023 in Wiley Online Library (<jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="http://wileyonlinelibrary.com">wileyonlinelibrary.com</jats:ext-link>), has been retracted by agreement between the journal's Editors in Chief, Ian D. Somerville and Yunpeng Dong; and John Wiley &amp; Sons Ltd. The retraction has been agreed following concerns raised by a third party. Further investigation by the publisher has found manipulation of the peer review process. The retraction is warranted due to the compromised integrity of the article's peer review.</jats:p>

<jats:p><jats:bold>RETRACTION</jats:bold>: H. Najam, “Optimization of renewable energy supply for a carbon neutral society: Role of environmental regulations, sustainable finance, and financial innovation through the lens of game theory,” <jats:italic>Geological Journal</jats:italic> 58, no. 9 (2023): 3466–3475, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="https://doi.org/10.1002/gj.4746">https://doi.org/10.1002/gj.4746</jats:ext-link>.</jats:p><jats:p>The above article, published online on 13 April 2023 in Wiley Online Library (<jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="http://wileyonlinelibrary.com">wileyonlinelibrary.com</jats:ext-link>), has been retracted by agreement between the journal's Editors in Chief, Ian D. Somerville and Yunpeng Dong; and John Wiley &amp; Sons Ltd. The retraction has been agreed following concerns raised by a third party. Further investigation by the publisher has found manipulation of the peer review process. The retraction is warranted due to the compromised integrity of the article's peer review.</jats:p>

<jats:p>During the early Cenozoic, the collision and convergence between India and Eurasia resulted in the uplift of the Tibetan Plateau and continuous northward compression, forming the Circum‐Tibetan Plateau Basin and Orogen System (CTPBOS). The Tarim Basin, located between the Tibetan Plateau and the Tianshan Mountains, plays a crucial role for studying the convergence‐driving strain propagation mechanism intra‐Asian continent during the growth processes of the Tibetan Plateau. Owing to the lack of accurate geophysical information on the deep structure of the Tarim crust，the mechanism of Cenozoic deformation in the Tarim Basin has been under debate. In this paper, the teleseismic data acquired by the broadband seismic profile across the Tarim Basin from south to north and the S‐wave receiver function method were used to obtain the depth of the Moho and the discontinuities in the lithosphere beneath the Tarim Basin. The SRF result shows that the Moho geometry has an abrupt relief under the Bachu Uplift, and Moho offset under the fault zone between the Kalashayi Fault and the Tumuxiuke Fault. The regional dip of the Moho under the Bachu area can be explained by the root of the Bachu basement‐involved uplift cutting across the whole crust and locally penetrating into the mantle lithosphere. The Bachu Uplift, located in the central Tarim terrane, has a relatively weak lithosphere. In the process of forming the Tarim large igneous province during the early Permian, the crust beneath the Bachu area was weakened and thinned by the thermo‐mechanical erosion from upwelling mantle plume. As the collision and convergence of India and Eurasia since the early Cenozoic, the convergence‐driving strain was propagated into the Tarim Basin. The pre‐existing weak Bachu Uplift was reactivated. The Tarim Basin absorbs Cenozoic compressional deformation through the crustal shortening and Moho offset of the Bachu Uplift.</jats:p>