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1

Wex, Sebastian, Neil S. Mancktelow, Friedrich Hawemann, Alfredo Camacho, and Giorgio Pennacchioni. "Inverted distribution of ductile deformation in the relatively “dry” middle crust across the Woodroffe Thrust, central Australia." Solid Earth 9, no. 4 (July 11, 2018): 859–78. http://dx.doi.org/10.5194/se-9-859-2018.

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Abstract. Thrust fault systems typically distribute shear strain preferentially into the hanging wall rather than the footwall. The Woodroffe Thrust in the Musgrave Block of central Australia is a regional-scale example that does not fit this model. It developed due to intracontinental shortening during the Petermann Orogeny (ca. 560–520 Ma) and is interpreted to be at least 600 km long in its E–W strike direction, with an approximate top-to-north minimum displacement of 60–100 km. The associated mylonite zone is most broadly developed in the footwall. The immediate hanging wall was only margi
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Camacho, A., B. Simons, and P. W. Schmidt. "Geological and palaeomagnetic significance of the Kulgera Dyke Swarm, Musgrave Block, NT, Australia." Geophysical Journal International 107, no. 1 (October 1991): 37–45. http://dx.doi.org/10.1111/j.1365-246x.1991.tb01154.x.

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Hawemann, Friedrich, Neil S. Mancktelow, Sebastian Wex, Alfredo Camacho, and Giorgio Pennacchioni. "Pseudotachylyte as field evidence for lower-crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)." Solid Earth 9, no. 3 (May 9, 2018): 629–48. http://dx.doi.org/10.5194/se-9-629-2018.

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Abstract. Geophysical evidence for lower continental crustal earthquakes in almost all collisional orogens is in conflict with the widely accepted notion that rocks, under high grade conditions, should flow rather than fracture. Pseudotachylytes are remnants of frictional melts generated during seismic slip and can therefore be used as an indicator of former seismogenic fault zones. The Fregon Subdomain in Central Australia was deformed under dry sub-eclogitic conditions of 600–700 °C and 1.0–1.2 GPa during the intracontinental Petermann Orogeny (ca. 550 Ma) and contains abundant pseudotachyly
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Kelly, Nigel M., Geoffrey L. Clarke, and Simon L. Harley. "Monazite behaviour and age significance in poly-metamorphic high-grade terrains: A case study from the western Musgrave Block, central Australia11Abbreviations: After Kretz, 1983." Lithos 88, no. 1-4 (May 2006): 100–134. http://dx.doi.org/10.1016/j.lithos.2005.08.007.

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Macnae, James, Xiuyan Ren, and Tim Munday. "Stripping induced polarization effects from airborne electromagnetics to improve 3D conductivity inversion of a narrow palaeovalley." GEOPHYSICS 85, no. 5 (July 7, 2020): B161—B167. http://dx.doi.org/10.1190/geo2019-0396.1.

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The electrical conductivity distribution within wide palaeochannels is usually well-mapped from airborne electromagnetic data using stitched 1D algorithms. Such stitched 1D solutions are, however, inappropriate for narrow valleys. An alternative option is to consider 2D or 3D models to allow for finite lateral extent of conductors. In airborne electromagnetic data within the Musgrave block near the well-studied Valen conductor, strong induced polarization (IP) and superparamagnetic (SPM) effects make physical property and structure estimation even more uncertain for deep channel clays, particu
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Fan, Xiao-Ping, Yi-Cheng He, Cong-Jie Yang, and Jun-Fei Wang. "Evaluation of crustal inhomogeneity parameters in the southern Longmenshan fault zone and adjacent regions." Journal of Seismology 24, no. 6 (August 19, 2020): 1175–88. http://dx.doi.org/10.1007/s10950-020-09949-w.

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AbstractBroadband teleseismic waveform data from 13 earthquakes recorded by 70 digital seismic stations were selected to evaluate the inhomogeneity parameters of the crustal medium in the southern Longmenshan fault zone and its adjacent regions using the teleseismic fluctuation wavefield method. Results show that a strong inhomogeneity exists beneath the study region, which can be divided into three blocks according to its structure and tectonic deformation features. These are known as the Sichuan-Qinghai Block, the Sichuan-Yunnan Block, and the Mid-Sichuan Block. The velocity fluctuation rati
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Smethurst, M. A., and J. C. Briden. "Palaeomagnetism of Silurian Sediments In W Ireland: Evidence For Block Rotation In the Caledonides." Geophysical Journal International 95, no. 2 (November 1, 1988): 327–46. http://dx.doi.org/10.1111/j.1365-246x.1988.tb00472.x.

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White, R. W., Roger Powell, and G. L. Clarke. "The interpretation of reaction textures in Fe-rich metapelitic granulites of the Musgrave Block, central Australia: constraints from mineral equilibria calculations in the system K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-Fe2O3." Journal of Metamorphic Geology 20, no. 1 (January 11, 2002): 41–55. http://dx.doi.org/10.1046/j.0263-4929.2001.00349.x.

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9

Bache, Francois, Paul Walshe, Juergen Gusterhuber, Sandra Menpes, Mattilda Sheridan, Sergey Vlasov, and Lance Holmes. "Exploration of the south-eastern part of the Frontier Amadeus Basin, Northern Territory, Australia." APPEA Journal 58, no. 1 (2018): 190. http://dx.doi.org/10.1071/aj17221.

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The Neoproterozoic to Late Paleozoic-aged Amadeus Basin is a large (~170 000 km2) east–west-trending basin, bounded to the south by the Musgrave Province and to the north by the Arunta Block of the Northern Territory. Commercial oil and gas production is established in the northern part of the basin but the southern part is still a frontier exploration area. Vintage and new seismic reflection data have been used with well data along the south-eastern Amadeus Basin to construct a new structural and depositional model. Three major phases of deformation controlling deposition have been identified
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10

Xu, Wenjing, Xisheng Xu, Yuejun Wang, and Matthew Jacek Brzozowski. "The effects of mafic-felsic magma interaction on magma diversity: insights from an early Paleozoic hornblendite-quartz monzonite suite in the South China block." Mineralogy and Petrology 114, no. 1 (January 7, 2020): 71–90. http://dx.doi.org/10.1007/s00710-019-00692-w.

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11

Yin, Rong, Li Han, Xiao-Long Huang, Jie Li, Wu-Xian Li, and Lin-Li Chen. "Textural and chemical variations of micas as indicators for tungsten mineralization: Evidence from highly evolved granites in the Dahutang tungsten deposit, South China." American Mineralogist 104, no. 7 (July 1, 2019): 949–65. http://dx.doi.org/10.2138/am-2019-6796.

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Abstract The Dahutang tungsten deposit, located in the Yangtze Block, South China, is one of the largest tungsten deposits in the world. Tungsten mineralization is closely related to Mesozoic granitic plutons. A drill core through a pluton in the Dalingshang ore block in the Central segment of the Dahutang tungsten deposit shows that the pluton is characterized by multi-stage intrusive phases including biotite granite, muscovite granite, and Li-mica granite. The granites are strongly peraluminous and rich in P and F. Decreasing bulk-rock (La/Yb)N ratios and total rare earth element (ΣREE) conc
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12

Sattarvand, Javad, and Christian Niemann-Delius. "A New Metaheuristic Algorithm for Long-Term Open-Pit Production Planning / Nowy meta-heurystyczny algorytm wspomagający długoterminowe planowanie produkcji w kopalni odkrywkowej." Archives of Mining Sciences 58, no. 1 (March 1, 2013): 107–18. http://dx.doi.org/10.2478/amsc-2013-0007.

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Paper describes a new metaheuristic algorithm which has been developed based on the Ant Colony Optimisation (ACO) and its efficiency have been discussed. To apply the ACO process on mine planning problem, a series of variables are considered for each block as the pheromone trails that represent the desirability of the block for being the deepest point of the mine in that column for the given mining period. During implementation several mine schedules are constructed in each iteration. Then the pheromone values of all blocks are reduced to a certain percentage and additionally the pheromone val
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13

Wadsworth, W. J. "Silicate mineralogy of the Behelvie cumulates, N E Scotland." Mineralogical Magazine 55, no. 378 (March 1991): 113–19. http://dx.doi.org/10.1180/minmag.1991.055.378.09.

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AbstractUltramafic, troctolitic and gabbroic rocks at the northern end of the Belhelvie layered intrusion display progressive cryptic variation over a stratigraphic thickness of approximately 800 m in steeply-dipping cumulates, which young from W to E. This variation is shown by olivine (Fo87−77), orthopyroxene (En87−79), clinopyroxene (Ca45Mg48Fe7 to Ca44.5Mg45.5Fe10) and plagioclase (An81−75). The Belhelvie succession is believed to be equivalent to the poorly-exposed and structurally complex Insch Lower Zone. A laterally impersistent hypersthene-gabbro unit within the main sequence is re-in
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14

Ismagilov, F. R., M. K. Dzheksenov, and A. V. Kurochkin. "Technology for Block Design of a Gas Treatment Plant for Oil Blow-Off to Remove Hydrogen Sulfide." Chemical and Petroleum Engineering 56, no. 7-8 (November 2020): 633–37. http://dx.doi.org/10.1007/s10556-020-00820-w.

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15

Hashemi, Seyed Ahmad, Bahram Rezai, Mohammad Reza Tavakoli Mohammadi, and Sepideh Javanshir. "Characterization and Concentration Studies of Jalal Abad Iron Mine / Charakterystyka I Badania Koncentracji W Kopalni Rud Żelaza Jalal Abad." Archives of Mining Sciences 58, no. 3 (September 1, 2013): 729–45. http://dx.doi.org/10.2478/amsc-2013-0051.

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Abstract Characterization and determination of liberation degree are the first stages of ore dressing. Block 4 of Jalal Abad mine, Kerman province, Iran, has three kinds of iron ores; D1, D2 and D3, with different grades. In this research, chemical analysis, mineralogy, liberation degree and magnetic enrichment studies were done by XRF, XRD, microscopic sections and Davis tube, respectively. The results indicated that D1, D2 and D3 had average iron grades of 58, 52 and 38%, respectively. The minerals of Magnetite, Hematite, Dolomite, Calcite and Quartz were distinguished. Average liberation de
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16

Frontera, T., A. Concha, P. Blanco, A. Echeverria, X. Goula, R. Arbiol, G. Khazaradze, F. Pérez, and E. Suriñach. "DInSAR Coseismic Deformation of the May 2011 M<sub>w</sub> 5.1 Lorca Earthquake (southeastern Spain)." Solid Earth 3, no. 1 (April 2, 2012): 111–19. http://dx.doi.org/10.5194/se-3-111-2012.

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Abstract. The coseismic superficial deformation at the region of Lorca (Murcia, southeastern Spain) due to the Mw 5.1 earthquake on 11 May 2011 was characterized by a multidisciplinary team, integrating information from DInSAR, GPS and numerical modelling techniques. Despite the moderate magnitude of the event, quantitative information was obtained from the interferometric study of a pair of TerraSAR-X images. The DinSAR results defined the trace of the fault plane and evidenced uplift of the hanging wall block in agreement with the estimated deformation obtained through an elastic rupture dis
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17

Wu, Chenglong, Tao Xu, Yinshuang Ai, Weiyu Dong, and Long Li. "XKS splitting-based upper-mantle deformation in the Jiaodong Peninsula records the boundary between the North China Craton and South China Block." Geophysical Journal International 222, no. 2 (May 9, 2020): 956–64. http://dx.doi.org/10.1093/gji/ggaa224.

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SUMMARY The Jiaodong Peninsula consists of the Jiaobei massif and the Northern Sulu UHP massif. These are separated by the Wulian suture zone (WSZ), a key region for understanding the collision between the North China Craton (NCC) and South China Block (SCB). To interpret this collisional zone, a broad-band seismic profile of 20 stations was installed across the WSZ. Shear wave splitting analysis of teleseismic data revealed a contrast in the splitting patterns beneath different structural zones of the Jiaodong Peninsula. The anisotropic structures of the Jiaobei massif and Northern Sulu UHP m
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18

Lee, Tien‐Chang, Thomas L. Henyey, and Brian N. Damiata. "A simple method for the absolute measurement of thermal conductivity of drill cuttings." GEOPHYSICS 51, no. 8 (August 1986): 1580–84. http://dx.doi.org/10.1190/1.1442208.

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We present a method for absolute measurement of thermal conductivity of drill cuttings. The simplicity of the apparatus makes it suitable for nondestructive use of cuttings and for sample sizes too small to be measured with a needle probe. Because the measurement is absolute, no calibration standards are required. Samples are placed in a Plexiglas cup with a lid containing an electric heat source. The base of the cup is placed in good thermal contact with an aluminum‐block heat sink. Upward and radial heat losses are minimized with styrofoam insulation surrounding the cup. The accuracy of the
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19

Ni, Pei, Guo-Guang Wang, Wen-Sheng Li, Zhe Chi, Su-Ning Li, and Yan Gao. "A review of the Yanshanian ore-related felsic magmatism and tectonic settings in the Nanling W-Sn and Wuyi Au-Cu metallogenic belts, Cathaysia Block, South China." Ore Geology Reviews 133 (June 2021): 104088. http://dx.doi.org/10.1016/j.oregeorev.2021.104088.

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Pautov, Leonid A., Atali A. Agakhanov, Vladimir Yu Karpenko, Yulia A. Uvarova, Elena Sokolova, and Frank C. Hawthorne. "Rinkite-(Y), Na2Ca4YTi(Si2O7)2OF3, a seidozerite-supergroup TS-block mineral from the Darai-Pioz alkaline massif, Tien-Shan mountains, Tajikistan: Description and crystal structure." Mineralogical Magazine 83, no. 03 (June 29, 2018): 373–80. http://dx.doi.org/10.1180/mgm.2018.122.

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AbstractRinkite-(Y), ideally Na2Ca4YTi(Si2O7)2OF3, is a new rinkite-group (seidozerite-supergroup) TS-block mineral from the Darai-Pioz alkaline massif, Tian-Shan mountains, Tajikistan. The mineral is of hydrothermal origin. It occurs as aggregates (up to 1.5 cm long) of acicular crystals 0.1–1.0 mm thick, and as separate elongated columnar, flattened-prismatic crystals up to 1 cm long with rectangular or rhombic sections up to 0.5 mm across. Associated minerals are quartz, aegirine, microcline, neptunite, pectolite, calcite, eudialyte-group minerals, fluorite, titanite, turkestanite, kupletsk
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21

Zhang, Zhi-Gang, Yan-Bao Liu, Hai-Tao Sun, Wei Xiong, Kai Shen, and Quan-Bin Ba. "An alternative approach to match field production data from unconventional gas-bearing systems." Petroleum Science 17, no. 5 (May 18, 2020): 1370–88. http://dx.doi.org/10.1007/s12182-020-00454-w.

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Abstract Nowadays, the unconventional gas-bearing system plays an increasingly important role in energy market. The performances of the current history-matching techniques are not satisfied when applied to such systems. To overcome this shortfall, an alternative approach was developed and applied to investigate production data from an unconventional gas-bearing system. In this approach, the fluid flow curve obtained from the field is the superposition of a series of Gaussian functions. An automatic computing program was developed in the MATLAB, and both gas and water field data collected from
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22

Shulgin, Alexey, Jan Inge Faleide, Rolf Mjelde, Asbjørn Breivik, and Ritske Huismans. "Crustal domains in the Western Barents Sea." Geophysical Journal International 221, no. 3 (April 24, 2020): 2155–69. http://dx.doi.org/10.1093/gji/ggaa112.

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SUMMARY The crustal architecture of the Barents Sea is still enigmatic due to complex evolution during the Timanian and Caledonian orogeny events, further complicated by several rifting episodes. In this study we present the new results on the crustal structure of the Caledonian–Timanian transition zone in the western Barents. We extend the work of Aarseth et al. (2017), by utilizing the seismic tomography approach to model Vp, Vs and Vp/Vs ratio, combined with the reprocessed seismic reflection line, and further complemented with gravity modelling. Based on our models we document in 3-D the p
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23

Torne, Montserrat, Ivone Jiménez–Munt, Jaume Vergés, Manel Fernàndez, Alberto Carballo, and Margarete Jadamec. "Regional crustal and lithospheric thickness model for Alaska, the Chukchi shelf, and the inner and outer bering shelves." Geophysical Journal International 220, no. 1 (October 7, 2019): 522–40. http://dx.doi.org/10.1093/gji/ggz424.

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SUMMARY This study presents for the first time an integrated image of the crust and lithospheric mantle of Alaska and its adjacent western shelves of the Chukchi and Bering seas based on joint modelling of potential field data constrained by thermal analysis and seismic data. We also perform 3-D forward modelling and inversion of Bouguer anomalies to analyse density heterogeneities at the crustal level. The obtained crustal model shows northwest-directed long wavelength thickening (32–36 km), with additional localized trends of thicker crust in the Brooks Range (40 km) and in the Alaska and St
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24

Gao, Wei, Ruizhong Hu, Albert H. Hofstra, Qiuli Li, Jingjing Zhu, Keqiang Peng, Lan Mu, Yong Huang, Jianwen Ma, and Qiang Zhao. "U-Pb Dating on Hydrothermal Rutile and Monazite from the Badu Gold Deposit Supports an Early Cretaceous Age for Carlin-Type Gold Mineralization in the Youjiang Basin, Southwestern China." Economic Geology 116, no. 6 (September 1, 2021): 1355–85. http://dx.doi.org/10.5382/econgeo.4824.

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Abstract The Youjiang basin on the southwestern margin of the Yangtze block in southwestern China is the world’s second largest Carlin-type gold province after Nevada, USA. The lack of precise age determinations on gold deposits in this province has hindered understanding of their genesis and relation to the geodynamic setting. Although most Carlin-type gold deposits in the basin are hosted in calcareous sedimentary rocks, ~70% of the ore in the Badu Carlin-type gold deposit is hosted by altered and sulfidized dolerite. Although in most respects Badu is similar to other Carlin-type gold deposi
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25

Andersson, Joel B. H., Tobias E. Bauer, and Edward P. Lynch. "Evolution of structures and hydrothermal alteration in a Palaeoproterozoic supracrustal belt: Constraining paired deformation–fluid flow events in an Fe and Cu–Au prospective terrain in northern Sweden." Solid Earth 11, no. 2 (April 17, 2020): 547–78. http://dx.doi.org/10.5194/se-11-547-2020.

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Abstract. An approximately 90 km long Palaeoproterozoic supracrustal belt in the northwestern Norrbotten ore province (northernmost Sweden) was investigated to characterize its structural components, assess hydrothermal alteration–structural geology correlations, and constrain a paired deformation–fluid flow evolution for the belt. New geological mapping of five key areas (Eustiljåkk, Ekströmsberg, Tjårrojåkka, Kaitum West, and Fjällåsen–Allavaara) indicates two major compressional events (D1 and D2) have affected the belt, with each associated with hydrothermal alteration types typical for ir
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26

Leitch, C. H. B., P. van der Heyden, C. I. Godwin, R. L. Armstrong, and J. E. Harakal. "Geochronometry of the Bridge River Camp, southwestern British Columbia." Canadian Journal of Earth Sciences 28, no. 2 (February 1, 1991): 195–208. http://dx.doi.org/10.1139/e91-019.

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Mineralization at the Bralorne mesothermal gold vein deposit is closely related to a suite of early Late Cretaceous to early Tertiary dykes. Premineral albitite dykes (91.4 ± 1.4 Ma by U–Pb on zircons) and postmineral lamprophyre dykes (43.5 ± 1.5 Ma by K–Ar on biotite) set definite age limits on the mineralizing event. A late intra- to post-mineral green hornblende dyke set (85.7 ± 3.0 Ma by K–Ar on hornblende) that forms a transitional series to the albitites may further restrict the age. Thus, mineralization occurred long after emplacement of the host Bralorne intrusions, dated as Early Per
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27

Hansen, Torsten Hundebøl, Ole Rønø Clausen, and Katrine Juul Andresen. "Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics." Solid Earth 12, no. 8 (August 4, 2021): 1719–47. http://dx.doi.org/10.5194/se-12-1719-2021.

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Abstract. Using borehole-constrained 3D reflection seismic data, we analyse the importance of sub-salt, salt, and supra-salt deformation in controlling the geometries and the kinematics of inverted structures in the Danish Central Graben. The Danish Central Graben is part of the failed Late Jurassic North Sea rift. Later tectonic shortening caused mild basin inversion during the Late Cretaceous and Paleogene. Where mobile Zechstein evaporites are present, they have played a significant role in the structural evolution of the Danish Central Graben since the Triassic. Within the study area, Jura
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28

Camacho, Alfredo, and John D. Fitz Gerald. "Misidentification of oxide phases and of twinned kyanite: implications for inferred P-T histories of the Musgrave Block, central Australia." Journal of the Virtual Explorer 35 (2010). http://dx.doi.org/10.3809/jvirtex.2011.00275.

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Wang, Yuan, Changsong Lin, Yanda Sun, Jingyan Liu, Hao Li, Haiquan He, Qinglong Wang, et al. "Depositional sequences and microfacies of Lower Carboniferous strata in the Marsel block of the Chu-Sarysu Basin, Southern Kazakhstan." Carbonates and Evaporites 35, no. 2 (March 18, 2020). http://dx.doi.org/10.1007/s13146-020-00573-w.

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