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Journal articles on the topic 'Tectonic evolution of Sulawesi'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Wakita, Koji, Jan Sopaheluwakan, Kazuhiro Miyazaki, Iskandar Zulkarnain, and Munasri. "Tectonic evolution of the Bantimala Complex, South Sulawesi, Indonesia." Geological Society, London, Special Publications 106, no. 1 (1996): 353–64. http://dx.doi.org/10.1144/gsl.sp.1996.106.01.23.

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2

Vane-Wright, RI. "Transcending the Wallace line: do the western edges of the Australina region and the Australian plate coincide?" Australian Systematic Botany 4, no. 1 (1991): 183. http://dx.doi.org/10.1071/sb9910183.

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The island of Sulawesi (Celebes), which lies at the heart of the Malay Archipelago, occurs in a region of exceptional tectonic complexity. Since Wallace first drew attention to the anomalous fauna of the island, debate has continued regarding the biogeography and geology of the area. Through an analysis of the distribution of the 183 genera and 470 species of butterflies known from Sulawesi (of which more than 200 species are regional endemics), two classes of biotic patterns linking the island to surrounding regions can be demonstrated. All, or virtually all of the genera on Sulawesi are Asian, but with no special link to Borneo. A set of younger patterns, derived from analysing species' distributions, links Sulawesi to the Moluccas, Philippines and the Lesser Sunda Islands, in addition to Asia. Of these younger patterns, the link between Sulawesi and the Moluccas is most pronounced . This is interpreted to suggest that current geological models, in which Sulawesi consists of at least two terranes, one Asian and one Australian in origin, are consistent with butterfly biogeography only if certain assumptions or constraints are imposed. Firstly, it must be assumed that Sulawesi has had a long independent history from Borneo; it seems most unlikely that Sulawesi and Borneo could have been contiguous 2 mya, as one geological theory has suggested. Secondly, before collision of the Asian and Australian plates about 15 mya, the advancing edge of the Australian plate must have been submerged during most if not all of the approach phase. If the collision has created new land by uplift in the eastern Sulawesi, Banggai and Sula region, then the strong species-level link between Sulawesi and the Moluccas is explicable by local dispersion over the last 15 mya. It is concluded that there is no sharp distinction, at least within Wallacea, between the Asian and Australian biota, as Wallace originally tried to demonstrate and as geological theories might predict: the western edges of the Australian biogeographic area and the Australian tectonic plate do not coincide.

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3

Surmont, J., C. Laj, C. Kissel, C. Rangin, H. Bellon, and B. Priadi. "New paleomagnetic constraints on the Cenozoic tectonic evolution of the North Arm of Sulawesi, Indonesia." Earth and Planetary Science Letters 121, no. 3-4 (February 1994): 629–38. http://dx.doi.org/10.1016/0012-821x(94)90096-5.

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4

Sendjaja, Purnama, Emmy Suparka, Chalid I. Abdullah, and IGB Eddy Sucipta. "Characteristic of the Mount Colo Volcano, Una-Una Island, Central Sulawesi Province: Tectonic Evolution and Disaster Mitigation." IOP Conference Series: Earth and Environmental Science 589 (November 19, 2020): 012005. http://dx.doi.org/10.1088/1755-1315/589/1/012005.

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5

Russell, James M., Satria Bijaksana, Hendrik Vogel, Martin Melles, Jens Kallmeyer, Daniel Ariztegui, Sean Crowe, et al. "The Towuti Drilling Project: paleoenvironments, biological evolution, and geomicrobiology of a tropical Pacific lake." Scientific Drilling 21 (July 27, 2016): 29–40. http://dx.doi.org/10.5194/sd-21-29-2016.

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Abstract. The Towuti Drilling Project (TDP) is an international research program, whose goal is to understand long-term environmental and climatic change in the tropical western Pacific, the impacts of geological and environmental changes on the biological evolution of aquatic taxa, and the geomicrobiology and biogeochemistry of metal-rich, ultramafic-hosted lake sediments through the scientific drilling of Lake Towuti, southern Sulawesi, Indonesia. Lake Towuti is a large tectonic lake at the downstream end of the Malili lake system, a chain of five highly biodiverse lakes that are among the oldest lakes in Southeast Asia. In 2015 we carried out a scientific drilling program on Lake Towuti using the International Continental Scientific Drilling Program (ICDP) Deep Lakes Drilling System (DLDS). We recovered a total of ∼ 1018 m of core from 11 drilling sites with water depths ranging from 156 to 200 m. Recovery averaged 91.7 %, and the maximum drilling depth was 175 m below the lake floor, penetrating the entire sedimentary infill of the basin. Initial data from core and borehole logging indicate that these cores record the evolution of a highly dynamic tectonic and limnological system, with clear indications of orbital-scale climate variability during the mid- to late Pleistocene.

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6

Zahirovic, S., M. Seton, and R. D. Müller. "The Cretaceous and Cenozoic tectonic evolution of Southeast Asia." Solid Earth 5, no. 1 (April 29, 2014): 227–73. http://dx.doi.org/10.5194/se-5-227-2014.

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Abstract. Tectonic reconstructions of Southeast Asia have given rise to numerous controversies that include the accretionary history of Sundaland and the enigmatic tectonic origin of the proto-South China Sea. We assimilate a diversity of geological and geophysical observations into a new regional plate model, coupled to a global model, to address these debates. Our approach takes into account terrane suturing and accretion histories, the location of subducted slabs imaged in mantle tomography in order to constrain the evolution of regional subduction zones, as well as plausible absolute and relative plate velocities and tectonic driving mechanisms. We propose a scenario of rifting from northern Gondwana in the latest Jurassic, driven by northward slab pull from north-dipping subduction of Tethyan crust beneath Eurasia, to detach East Java, Mangkalihat, southeast Borneo and West Sulawesi blocks that collided with a Tethyan intra-oceanic subduction zone in the mid-Cretaceous and subsequently accreted to the Sunda margin (i.e., southwest Borneo core) in the Late Cretaceous. In accounting for the evolution of plate boundaries, we propose that the Philippine Sea plate originated on the periphery of Tethyan crust forming this northward conveyor. We implement a revised model for the Tethyan intra-oceanic subduction zones to reconcile convergence rates, changes in volcanism and the obduction of ophiolites. In our model the northward margin of Greater India collides with the Kohistan–Ladakh intra-oceanic arc at ∼53 Ma, followed by continent–continent collision closing the Shyok and Indus–Tsangpo suture zones between ∼42 and 34 Ma. We also account for the back-arc opening of the proto-South China Sea from ∼65 Ma, consistent with extension along east Asia and the formation of supra-subduction zone ophiolites presently found on the island of Mindoro. The related rifting likely detached the Semitau continental fragment from South China, which accreted to northern Borneo in the mid-Eocene, to account for the Sarawak Orogeny. Rifting then re-initiated along southeast China by 37 Ma to open the South China Sea, resulting in the complete consumption of proto-South China Sea by ∼17 Ma when the collision of the Dangerous Grounds and northern Palawan blocks with northern Borneo choked the subduction zone to result in the Sabah Orogeny and the obduction of ophiolites in Palawan and Mindoro. We conclude that the counterclockwise rotation of Borneo was accommodated by oroclinal bending consistent with paleomagnetic constraints, the curved lithospheric lineaments observed in gravity anomalies of the Java Sea and the curvature of the Cretaceous Natuna paleo-subduction zone. We complete our model by constructing a time-dependent network of topological plate boundaries and gridded paleo-ages of oceanic basins, allowing us to compare our plate model evolution to seismic tomography. In particular, slabs observed at depths shallower than ∼1000 km beneath northern Borneo and the South China Sea are likely to be remnants of the proto-South China Sea basin.

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7

Zahirovic, S., M. Seton, and R. D. Müller. "The Cretaceous and Cenozoic tectonic evolution of Southeast Asia." Solid Earth Discussions 5, no. 2 (August 21, 2013): 1335–422. http://dx.doi.org/10.5194/sed-5-1335-2013.

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Abstract. Tectonic reconstructions of Southeast Asia have given rise to numerous controversies which include the accretionary history of Sundaland and the enigmatic tectonic origin of the Proto South China Sea. We assimilate a diversity of geological and geophysical observations into a new regional plate model, coupled to a global model, to address these debates. Our approach takes into account terrane suturing and accretion histories, the location of subducted slabs imaged in mantle tomography in order to constrain the opening and closure history of paleo-ocean basins, as well as plausible absolute and relative plate velocities and tectonic driving mechanisms. We propose a scenario of rifting from northern Gondwana in the Late Jurassic, driven by northward slab pull, to detach East Java, Mangkalihat, southeast Borneo and West Sulawesi blocks that collided with a Tethyan intra-oceanic subduction zone in the mid Cretaceous and subsequently accreted to the Sunda margin (i.e. southwest Borneo core) in the Late Cretaceous. In accounting for the evolution of plate boundaries, we propose that the Philippine Sea Plate originated on the periphery of Tethyan crust forming this northward conveyor. We implement a revised model for the Tethyan intra-oceanic subduction zones to reconcile convergence rates, changes in volcanism and the obduction of ophiolites. In our model the northward margin of Greater India collides with the Kohistan-Ladakh intra-oceanic arc at ∼53 Ma, followed by continent-continent collision closing the Shyok and Indus-Tsangpo suture zones between ∼42 and 34 Ma. We also account for the back-arc opening of the Proto South China Sea from ∼65 Ma, consistent with extension along east Asia and the emplacement of supra-subduction zone ophiolites presently found on the island of Mindoro. The related rifting likely detached the Semitau continental fragment from east China, which accreted to northern Borneo in the mid Eocene, to account for the Sarawak Orogeny. Rifting then re-initiated along southeast China by 37 Ma to open the South China Sea, resulting in the complete consumption of Proto South China Sea by ∼17 Ma when the collision of the Dangerous Grounds and northern Palawan blocks with northern Borneo choked the subduction zone to result in the Sabah Orogeny and the obduction of ophiolites in Palawan and Mindoro. We conclude that the counterclockwise rotation of Borneo was accommodated by oroclinal bending consistent with paleomagnetic constraints, the curved lithospheric lineaments observed in gravity anomalies of the Java Sea and the curvature of the Cretaceous Natuna paleo-subduction zone. We complete our model by constructing a time-dependent network of continuously closing plate boundaries and gridded paleo-ages of oceanic basins, allowing us to test our plate model evolution against seismic tomography. In particular, slabs observed at depths shallower than ∼1000 km beneath northern Borneo and the South China Sea are likely to be remnants of the Proto South China Sea basin.

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8

van Leeuwen, Theo M., and Muhardjo. "Stratigraphy and tectonic setting of the Cretaceous and Paleogene volcanic-sedimentary successions in northwest Sulawesi, Indonesia: implications for the Cenozoic evolution of Western and Northern Sulawesi." Journal of Asian Earth Sciences 25, no. 3 (June 2005): 481–511. http://dx.doi.org/10.1016/j.jseaes.2004.05.004.

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9

Jablonski, D., and A. J. Saitta. "PERMIAN TO LOWER CRETACEOUS PLATE TECTONICS AND ITS IMPACT ON THE TECTONO-STRATIGRAPHIC DEVELOPMENT OF THE WESTERN AUSTRALIAN MARGIN." APPEA Journal 44, no. 1 (2004): 287. http://dx.doi.org/10.1071/aj03011.

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The post-Lower Permian succession of the Perth Basin and Westralian Superbasin can be directly related to the plate tectonic evolution of the Gondwanan Super-continent. In the Late Permian to Albian the northern edge of Gondwana continued to break into microplates that migrated to the north and were accreted into what is today the southeastern Asia (Burma–China) region. These separation events are recorded as a series of stratigraphically distinct transgressions (corresponding to the initial stretching of the asthenosphere and acceleration of subsidence rates) followed by rapid regressions (when new oceanic crust was emplaced in thinned continental crust causing uplifts of large continental masses). Because the events are synchronous across large regions, and may be identified from specific log and seismic signatures, the intensity of stratigraphically related transgressive/regressive cycles varies, depending on the distance from the break-up centres and these cycles allow the identification of regionally significant megasequences even in undrilled areas. The tectonic evolution and resulting stratigraphy can be described by eight plate tectonic events:Visean (Carboniferous) break-up of the southeastern Asia (Simao, Indochina and South China);Kungurian (uppermost Early Permian) break-up of Qiangtang and Sibumasu;Lowermost Norian uplift due to Bowen Orogeny in eastern Australia;Hettangian break-up of Mangkalihat (northeastern Borneo);Oxfordian break-up of Argo/West Burma, and Sikuleh (Western Sumatra);Kimmeridgian break-up of the West Sulawesi microplate;Tithonian break-up of Paternoster-Meratus (central Borneo); andValanginian break-up of Greater India/India.These events should be identifiable in all Australian Phanerozoic basins and beyond, potentially providing a template for a synchronisation of the Permian to Early Cretaceous stratigraphy.

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10

Bergman, Steven C., Dana Q. Coffield, James P. Talbot, and Richard A. Garrard. "Tertiary Tectonic and magmatic evolution of western Sulawesi and the Makassar Strait, Indonesia: evidence for a Miocene continent-continent collision." Geological Society, London, Special Publications 106, no. 1 (1996): 391–429. http://dx.doi.org/10.1144/gsl.sp.1996.106.01.25.

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11

Harum, Siva Dwi, Elvan Yuniarti, and Dwi Haryanto. "Pemodelan 2-Dimensi dan 3-Dimensi Penyebaran Bijih Besi Menggunakan Data Resistivitas dan IP di Daerah “A” Provinsi Kalimantan Selatan." Al-Fiziya: Journal of Materials Science, Geophysics, Instrumentation and Theoretical Physics 2, no. 1 (June 22, 2019): 56–63. http://dx.doi.org/10.15408/fiziya.v2i1.11175.

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Sulawesi Island is composed of complex tectonic arrangements. Most earthquake activities in Sulawesi are affected by the Palu - Koro Fault and Matano Fault. Palu - Koro Fault and Matano Fault are one of the faults in Central Sulawesi. Active movement of the fault results in high earthquake activity in the region of Central Sulawesi and its surroundings. This makes the importance of earthquake parameters in Central Sulawesi and surrounding areas. One of the efforts to find out earthquake parameter information accurately is to relocate. The purpose of this study was to conduct hypocenter earthquake relocation and determine the 1-D velocity structure of P waves in Central and surrounding areas using the Coupled Velocity - Hypocenter method with Velest 3.3 software. The data used are tectonic earthquake data from November 2009 to March 2018, data recording stations, and initial speed data. The results of data processing using the Velest 3.3 software are that some of the results of the relocation are close to fault, the final Vp at a depth of 9 km is slower than the initial Vp, the correction of the station obtained in this calculation is in the interval -0.81 to +0.54.

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12

Azizah, Lusti Nur, Arif Tjahjono, and Agung Sabtaji. "Relokasi Hiposenter Gempa Bumi dan Model Struktur Kecepatan 1 Dimensi Gelombang P dengan Menggunakan Metode Coupled Velocity – Hypocenter di Daerah Sulawesi Tengah dan Sekitarnya." Al-Fiziya: Journal of Materials Science, Geophysics, Instrumentation and Theoretical Physics 2, no. 1 (June 22, 2019): 1–9. http://dx.doi.org/10.15408/fiziya.v2i1.9514.

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Sulawesi Island is composed of complex tectonic arrangements. Most earthquake activities in Sulawesi are affected by the Palu - Koro Fault and Matano Fault. Palu - Koro Fault and Matano Fault are one of the faults in Central Sulawesi. Active movement of the fault results in high earthquake activity in the region of Central Sulawesi and its surroundings. This makes the importance of earthquake parameters in Central Sulawesi and surrounding areas. One of the efforts to find out earthquake parameter information accurately is to relocate. The purpose of this study was to conduct hypocenter earthquake relocation and determine the 1-D velocity structure of P waves in Central and surrounding areas using the Coupled Velocity - Hypocenter method with Velest 3.3 software. The data used are tectonic earthquake data from November 2009 to March 2018, data recording stations, and initial speed data. The results of data processing using the Velest 3.3 software are that some of the results of the relocation are close to fault, the final Vp at a depth of 9 km is slower than the initial Vp, the correction of the station obtained in this calculation is in the interval -0.81 to +0.54.

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13

Kaharuddin, MS, A. M. Imran, Chalid Idham Abdullah, and Asri Jaya. "Olistostrome and the mesozoic tectonic of the bantimala complex, South Sulawesi." MATEC Web of Conferences 101 (2017): 04011. http://dx.doi.org/10.1051/matecconf/201710104011.

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14

Massinai, Muhammad Altin, Muhammad Fawzy Ismullah Massinai, Mustakima, and Erfan Syamsuddin. "Present-day Tectonic Regime from Focal Mechanism Data in South Sulawesi." IOP Conference Series: Earth and Environmental Science 279 (September 5, 2019): 012016. http://dx.doi.org/10.1088/1755-1315/279/1/012016.

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15

Metcalfe, Ian. "Tectonic evolution of Sundaland." Bulletin of the Geological Society of Malaysia 63 (June 1, 2017): 27–60. http://dx.doi.org/10.7186/bgsm63201702.

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16

Barber, A. J., M. J. Crow, and M. E. M. De Smet. "Chapter 14 Tectonic Evolution." Geological Society, London, Memoirs 31, no. 1 (2005): 234–59. http://dx.doi.org/10.1144/gsl.mem.2005.031.01.14.

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17

Elburg, Marlina A., and John Foden. "Geochemical response to varying tectonic settings: an example from southern Sulawesi (Indonesia)." Geochimica et Cosmochimica Acta 63, no. 7-8 (April 1999): 1155–72. http://dx.doi.org/10.1016/s0016-7037(98)00298-1.

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18

Helmers, H., J. Sopaheluwakan, E. Surya Nila, and S. Tjokrosapoetro. "Blueschist evolution is Southeast Sulawesi, Indonesia." Netherlands Journal of Sea Research 24, no. 2-3 (November 1989): 373–81. http://dx.doi.org/10.1016/0077-7579(89)90162-2.

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19

Kapojos, Cloudya Gabriella, Gerald Tamuntuan, and Guntur Pasau. "ANALISIS PERCEPATAN TANAH MAKSIMUM DENGAN MENGGUNAKAN RUMUSAN ESTEVA DAN DONOVAN (Studi Kasus Pada Semenanjung Utara Pulau Sulawesi)." JURNAL ILMIAH SAINS 17, no. 1 (August 14, 2015): 99. http://dx.doi.org/10.35799/jis.15.2.2015.9225.

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ANALISIS PERCEPATAN TANAH MAKSIMUM DENGAN MENGGUNAKAN RUMUSAN ESTEVA DAN DONOVAN (Studi Kasus Pada Semenanjung Utara Pulau Sulawesi) ABSTRAK Telah dilakukan analisis percepatan tanah maksimum di semenanjung utara Pulau Sulawesi dengan menggunakan rumusan Esteva dan rumusan Donovan. Data yang digunakan adalah data gempa bumi tektonik yang terjadi di sekitar semenanjung utara Pulau Sulawesi pada periode tahun 2008 – 2014. Hasil analisis menunjukkan bahwa perubahan nilai percepatan tanah dari rumusan Esteva dan rumusan Donovan memiliki pola perubahan yang sama terhadap jarak. Nilai percepatan tanah menurut rumusan Donovan lebih tinggi dibandingkan dari rumusan Esteva. Perbandingan dengan data akselerograf mengindikasikan bahwa rumusan Esteva lebih cocok digunakan dalam mengestimasi percepatan tanah maksimum di semenanjung utara Pulau Sulawesi. Hasil pemetaan sebaran percepatan tanah maksimum menunjukkan bahwa wilayah Kabupaten Minahasa Utara berada pada zona dengan resiko yang lebih tinggi dibandingkan wilayah lainnya di semenanjung utara Pulau Sulawesi. Kata Kunci :Percepatan tanah maksimum, gempa bumi, semenanjung utara Pulau Sulawesi ANALYSIS OF PEAK GROUND ACCELERATION USING ESTEVA AND DONOVAN FORMULATIONS (A Case Study On The Northern Part of Sulawesi) ABSTRACT Peak ground acceleration on the northern part of Sulawesi Island has been analysis by using Esteva and Donovan formulations. We use tectonic earthquake data that occurred around the northern part of Sulawesi Island during period of 2008 till 2014. The results showed that both Esteva and Donovan formulations have the similar pattern on changes of peak ground acceleration to the distance. Value of peak ground acceleration calculated with Donovan method higher than Esteva method. Comparison between empirical formula results and accelerograf data show that Esteva formulation more suitable for use in estimating the peak ground acceleration in the northern part of Sulawesi Island. Distribution of peak ground acceleration indicate that the earthquake impact on North Minahasa Regency is higher than other regions in northern part of Sulawesi island. Keynotes: Peak Ground Acceleration, Earthquake, Northern Part of Sulawesi Island

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20

Hutchison, Charles S. "Tectonic evolution of Southeast Asia." Bulletin of the Geological Society of Malaysia 60 (December 1, 2014): 1–18. http://dx.doi.org/10.7186/bgsm60201401.

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21

Lee, Tung-Yi. "Tectonic evolution of Southeast Asia." Tectonophysics 270, no. 3-4 (March 1997): 327–28. http://dx.doi.org/10.1016/s0040-1951(96)00214-4.

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22

Sladen, Chris. "Tectonic evolution of Southeast Asia." Marine and Petroleum Geology 14, no. 5 (August 1997): 608. http://dx.doi.org/10.1016/s0264-8172(97)81119-1.

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23

Kidd, William S. F. "The tectonic evolution of Asia." Journal of Structural Geology 19, no. 11 (November 1997): 1438–39. http://dx.doi.org/10.1016/s0191-8141(97)80937-6.

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24

Burke, K. "Tectonic Evolution of the Caribbean." Annual Review of Earth and Planetary Sciences 16, no. 1 (May 1988): 201–30. http://dx.doi.org/10.1146/annurev.ea.16.050188.001221.

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25

Choukroune, P. "Tectonic Evolution of the Pyrenees." Annual Review of Earth and Planetary Sciences 20, no. 1 (May 1992): 143–58. http://dx.doi.org/10.1146/annurev.ea.20.050192.001043.

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26

Myers, John S., Russell D. Shaw, and Ian M. Tyler. "Tectonic evolution of Proterozoic Australia." Tectonics 15, no. 6 (December 1996): 1431–46. http://dx.doi.org/10.1029/96tc02356.

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27

Lee, Tung-Yi. "The Tectonic Evolution of Asia." Eos, Transactions American Geophysical Union 78, no. 50 (1997): 586. http://dx.doi.org/10.1029/97eo00356.

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28

Searle, Mike. "Tectonic evolution of southeast Asia." Journal of Structural Geology 18, no. 9 (September 1996): 1181. http://dx.doi.org/10.1016/0191-8141(96)82776-3.

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29

Windley, Brian. "The Tectonic Evolution of Asia." Geophysical Journal International 129, no. 1 (April 1997): 219. http://dx.doi.org/10.1111/j.1365-246x.1997.tb00954.x.

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30

Shackleton, R. M. "Tectonic evolution of greenstone belts." Geological Society, London, Special Publications 95, no. 1 (1995): 53–65. http://dx.doi.org/10.1144/gsl.sp.1995.095.01.04.

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31

Froidevaux, Claude, and Yanick Ricard. "Tectonic evolution of high plateaus." Tectonophysics 134, no. 1-3 (March 1987): 227–38. http://dx.doi.org/10.1016/0040-1951(87)90259-9.

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32

Tongkul, F. "Tectonic evolution of Sabah, Malaysia." Journal of Southeast Asian Earth Sciences 6, no. 3-4 (October 1991): 395–405. http://dx.doi.org/10.1016/0743-9547(91)90084-b.

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33

黄, 聿晓. "Tectonic Styles and Tectonic Evolution of Salin Depression in Myanmar." Advances in Geosciences 08, no. 02 (2018): 392–405. http://dx.doi.org/10.12677/ag.2018.82042.

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34

Villeneuve, Michel, Jean-Jacques Cornee, Wahyu Gunawan, Rossana Martini, Guy Tronchetti, Marie-Christine Janin, Pierre Saint-Marc, and Louisette Zaninetti. "La succession lithostratigraphique du bloc de Banda dans la region de Kolonodale (Sulawesi central, Indonesie)." Bulletin de la Société Géologique de France 172, no. 1 (January 1, 2001): 59–68. http://dx.doi.org/10.2113/172.1.59.

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Abstract Sulawesi island is the convergence area of the Eurasian, the Pacific and the Australian plates. Villeneuve et al. demonstrated, from both lithostratigraphic and tectonic studies, that east and southeast Sulawesi was composed of two major continental blocks. - The "Banda block", including also Buru, Seram and Sinta Ridge, collided with the Asian volcanic arc of west Sulawesi during Oligocene times, then was dismembered during the Late Neogene Banda sea opening. - The Banggai-Sula block which was drifted from Irian Jaya and collided with the Banda block during Mid-Late Pliocene times. One of the fragments of the Banda block is in East Sulawesi, corresponding to the ophiolitic zone. There, in the Kolonodale area, it is possible to reconstruct the sedimentary succession under the ophiolite, despite intensive deformations. Over several years the stratigraphic framework of this area was detailed, following general mapping, and it is now possible, by including unpublished data concerning Cainozoic rocks, to reconstruct the Mesozoic-Cainozoic succession. Reconstructing the succession was possible by joint structural, stratigraphic and palaeoenvironmental studies. An example of structural cross-sections around the Kolonodale gulf is given on figure 4, from which local successions were built. We can now propose the general succession.

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35

Wilson, Moyra E. J., and Steve J. Moss. "Cenozoic palaeogeographic evolution of Sulawesi and Borneo." Palaeogeography, Palaeoclimatology, Palaeoecology 145, no. 4 (February 1999): 303–37. http://dx.doi.org/10.1016/s0031-0182(98)00127-8.

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36

TAKENAKA, Osamu. "Origin and Evolution of the Sulawesi Macaque." Primate Research 2, no. 1 (1986): 21–24. http://dx.doi.org/10.2354/psj.2.21.

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37

KAWAMOTO, Yoshi. "Origin and Evolution of the Sulawesi Macaques." Primate Research 2, no. 1 (1986): 25–29. http://dx.doi.org/10.2354/psj.2.25.

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38

Horoiwa, Mizuki, Ixchel F. Mandagi, Nobu Sutra, Javier Montenegro, Fadly Y. Tantu, Kawilarang W. A. Masengi, Atsushi J. Nagano, Junko Kusumi, Nina Yasuda, and Kazunori Yamahira. "Mitochondrial introgression by ancient admixture between two distant lacustrine fishes in Sulawesi Island." PLOS ONE 16, no. 6 (June 10, 2021): e0245316. http://dx.doi.org/10.1371/journal.pone.0245316.

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Sulawesi, an island located in a biogeographical transition zone between Indomalaya and Australasia, is famous for its high levels of endemism. Ricefishes (family Adrianichthyidae) are an example of taxa that have uniquely diversified on this island. It was demonstrated that habitat fragmentation due to the Pliocene juxtaposition among tectonic subdivisions of this island was the primary factor that promoted their divergence; however, it is also equally probable that habitat fusions and resultant admixtures between phylogenetically distant species may have frequently occurred. Previous studies revealed that some individuals of Oryzias sarasinorum endemic to a tectonic lake in central Sulawesi have mitochondrial haplotypes that are similar to the haplotypes of O. eversi, which is a phylogenetically related but geologically distant (ca. 190 km apart) adrianichthyid endemic to a small fountain. In this study, we tested if this reflects ancient admixture of O. eversi and O. sarasinorum. Population genomic analyses of genome-wide single-nucleotide polymorphisms revealed that O. eversi and O. sarasinorum are substantially reproductively isolated from each other. Comparison of demographic models revealed that the models assuming ancient admixture from O. eversi to O. sarasinorum was more supported than the models assuming no admixture; this supported the idea that the O. eversi-like mitochondrial haplotype in O. sarasinorum was introgressed from O. eversi. This study is the first to demonstrate ancient admixture of lacustrine or pond organisms in Sulawesi beyond 100 km. The complex geological history of this island enabled such island-wide admixture of lacustrine organisms, which usually experience limited migration.

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39

Parkinson, Christopher D. "The origin and significance of metamorphosed tectonic blocks in mélanges: evidence from Sulawesi, Indonesia." Terra Nova 8, no. 4 (July 1996): 312–23. http://dx.doi.org/10.1111/j.1365-3121.1996.tb00564.x.

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40

Sukadana, I. Gde, Agung Harijoko, and Lucas Donny Setijadji. "Tataan Tektonika Batuan Gunung Api di Komplek Adang Kabupaten Mamuju Provinsi Sulawesi Barat." EKSPLORIUM 36, no. 1 (May 30, 2015): 31. http://dx.doi.org/10.17146/eksplorium.2015.36.1.2769.

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Kompleks batuan gunung api Adang di daerah Kabupaten Mamuju, Sulawesi Barat secara lebih detail dapat dikelompokkan menjadi tujuh, yaitu kompleks Tapalang, Ampalas, Adang, Malunda, Karampuang, Sumare, dan Labuan Rano. Komplek Adang merupakan salah satu komplek gunungapi utama yang masih dapat diidentifikasi bentukan morfologinya dengan baik. Komplek ini tersusunatas batuan gunung api basa hingga intermediet yang memiliki nilai laju dosis radiasi cukup tinggi yang disebabkan oleh kandungan mineral radioaktif di dalamnya. Keterdapatan mineral radioaktif pada batuan basaltik-andesitik belum pernah dijumpai di Indonesia sehingga hal ini menjadi sangat menarik untuk dilakukan penelitian terutama tataan tektonika pembentukan batuan komplek gunung api tersebut. Tujuan penelitian ini adalah untuk menentukan tipologi magmatik yang terkait dengantataan tektonikanya dengan pendekatan geokimia batuan gunung api menggunakan analisis X-Ray Fluorescence (XRF). Batuan gunung api Adang merupakan hasil dari proses vulkanisme suatu komplekgunung api yang memiliki pusat erupsi dan beberapa kubah lava. Batuan tersebut tersusun atas batuan trachyte-phonolite, dengan afinitas magmatiknya ultrapotasik, Dari data tersebut dapat diinterpretasi bahwa tataan tektonika magmatologinya adalah active continental margin(ACM). Magma asal yang membentuknya dari aktivitas gunung apinya dipengaruhi oleh kerak benua mikro barat daya (South West/SW) Sulawesi. Adang volcanic complexlocated in Mamuju Region, West Sulawesi can be grouped more detail into seven complexes that are Tapalang, Ampalas, Adang, Malunda, Karampuang, Sumare, and Labuan Rano. Adang complex is one of the main volcanic complexes that still can be identified with good morphological formations. This complex is composed of alkaline volcanic rocks with basic to intermediates composition that have high value of radiation dose rate caused by their radioactive mineral content. Radioactive mineral occurrences on the basaltic-andesitic rocks has never been found in Indonesia, so it becomes very interesting to do research mainly tectonic settings of the volcanic rock complex formation. The purpose of this study is to determine magmatiic typology related with the tectonic setting based on volcanic rock geochemistry using X-Ray Fluorences (XRF) analysis. Adang volcanic rock is the result of a complex process of volcanism having a volcanic center and several lava domes. They are composed of phonolite to dacite rock, with ultrapotassic affinity, interpretation of data concluded that tectonic setting of magmatism formed in active continental margin (ACM). Magmatism source from vulcanic activities influenced by South WestSulawesi micro-continental crust.

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Zhang, Ruigang, Jinhua Luan, Yang Chen, Fei Chen, and Yongwang Liu. "Tectonic Characteristics of the East Sichuan Basin and Regional Tectonic Evolution Characteristics of Regional Tectonic Belt." IOP Conference Series: Earth and Environmental Science 558 (September 5, 2020): 032009. http://dx.doi.org/10.1088/1755-1315/558/3/032009.

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42

Saputro, Sugeng Purwo, Dwi Ratih Purwaningsih, and Bambang Priadi. "Peralihan Rezim Tektonik: Implikasinya pada Konsentrasi Torium di Mamasa dan Tana Toraja, Sulawesi-Indonesia." EKSPLORIUM 41, no. 2 (November 30, 2020): 87. http://dx.doi.org/10.17146/eksplorium.2020.41.2.6063.

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ABSTRAK Mamasa dan Tana Toraja secara geografis merupakan bagian dari lengan barat Pulau Sulawesi. Batuan-batuan mafik di daerah tersebut dan sekitarnya memiliki nilai laju radiasi tinggi dan anomali kandungan torium (Th). Penelitian ini bertujuan untuk mengetahui mekanisme tataan tektonik yang berperan dalam peningkatan konsentrasi Th. Enam sampel batuan dianalisis menggunakan analisis petrografi dan geokimia (AAS, ICP-MS, NA, dan XRF), dilengkapi dengan pentarikhan umur menggunakan metode 40K-40Ar pada sampel batuan terpilih. Pengamatan petrografi memperlihatkan kehadiran mineral plagioklas, olivin, piroksen, hornblenda, nefelin, dan alanit pada batuan yang diidentifikasi sebagai nefelin-basanit, basalt, trakhibasalt, dan gabro. Sejumlah tekstur yang tampak pada batuan tersebut mengindikasikan kontaminasi dan perubahan kondisi tektonik. Analisis geokimia menunjukkan bahwa nefelin-basanit, basalt, trakhibasalt, dan gabro (absarokit) terbentuk pada batas kontinental aktif (ACM) yang sedang mengalami transisi dari subduksi aktif (penunjaman ke arah barat) menjadi post-subduksi. Perubahan tataan tektonik membuat magma membeku pada kondisi yang sangat ekstrim. Proses pembekuan magma diinterpretasikan terjadi pada umur sekitar 13,10-11,02 Ma. Mekanisme tersebut berperan penting terhadap terjadinya peningkatan konsentrasi torium di Mamasa dan Tana Toraja.ABSTRACT Mamasa and Tana Toraja geographically are part of the western arm of Sulawesi Island. The mafic rocks in these areas and their surroundings have high radiation dose rate and thorium (Th) anomaly content. This research aim is to determine tectonic setting mechanism which play the important role on the increasing of Th concentration. Six rock samples were analysed using petrography and geochemical analyses (AAS, ICP-MS, NA, and XRF) completed with the 40K-40Ar dating on selected rock samples. Petrography observations show plagioclase, olivine, pyroxene, hornblende, nepheline, and allanite minerals presence in the rocks which identified as nepheline-basanite, basalt, trachybasalt, and gabbro. Numbers of texture appearances in the rocks indicate contamination and changes on tectonic setting. Geochemistry analysis shows that nepheline-basanite, basalt, trachybasalt, and gabbro (absarokite) were formed at the active continental margin (ACM), which is undergoing active subduction (westward subduction) to post-subduction transition. The changing of tectonic setting made magma solidify in extreme conditions. The magma solidify process is interpreted to occur at the age of 13.10-11.02 Ma. These mechanisms play an important role for the increase of thorium concentration in Mamasa and Tana Toraja.

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Gaulier, J. M., and P. Huchon. "Tectonic evolution of Afar triple junction." Bulletin de la Société Géologique de France 162, no. 3 (May 1, 1991): 451–64. http://dx.doi.org/10.2113/gssgfbull.162.3.451.

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Davies, Geoffrey F. "Punctuated tectonic evolution of the earth." Earth and Planetary Science Letters 136, no. 3-4 (December 1995): 363–79. http://dx.doi.org/10.1016/0012-821x(95)00167-b.

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Phillips, R. J., and V. L. Hansen. "Tectonic and Magmatic Evolution of Venus." Annual Review of Earth and Planetary Sciences 22, no. 1 (May 1994): 597–656. http://dx.doi.org/10.1146/annurev.ea.22.050194.003121.

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46

Metcalfe, I. "Tectonic evolution of the Malay Peninsula." Journal of Asian Earth Sciences 76 (October 2013): 195–213. http://dx.doi.org/10.1016/j.jseaes.2012.12.011.

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Ramos, Victor A., and Manuel Moreno. "Tectonic evolution of the Colombian Andes." Journal of South American Earth Sciences 21, no. 4 (September 2006): 319–21. http://dx.doi.org/10.1016/j.jsames.2006.07.008.

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48

McGill, George E. "Hotspot evolution and Venusian tectonic style." Journal of Geophysical Research: Planets 99, E11 (November 25, 1994): 23149–61. http://dx.doi.org/10.1029/94je02319.

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49

Naar, David F., and R. N. Hey. "Tectonic evolution of the Easter Microplate." Journal of Geophysical Research 96, B5 (1991): 7961. http://dx.doi.org/10.1029/90jb02398.

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50

Hall, Robert, D. J. Blundell, and Robert Hall. "Tectonic evolution of SE Asia: introduction." Geological Society, London, Special Publications 106, no. 1 (1996): vii—xiii. http://dx.doi.org/10.1144/gsl.sp.1996.106.01.01.

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