Plate tectonics and the development of sedimentary basins of the dextral regime in western Southeast Asia

1993 ◽  
Vol 8 (1-4) ◽  
pp. 497-511 ◽  
Author(s):  
Gordon H Packham
Keyword(s):  
Southeast Asia ◽  
Plate Tectonics ◽  
Sedimentary Basins

The Geological Framework

2005 ◽  
Author(s):  
Charles S. Hutchison
Keyword(s):  
Indian Ocean ◽  
Southeast Asia ◽  
Deep Water ◽  
Plate Tectonics ◽  
Petroleum Industry ◽  
South Indian ◽  
Lithospheric Plates ◽  
Asean Countries ◽  
Convergent Plate Margin ◽  
Straits Of Malacca

This chapter outlines the principal geological features of the region, extending from Myanmar and Taiwan in the north, southwards to include all the ASEAN countries, and extending as far as northern Australia. The present-day lithospheric plates and plate margins are described, and the Cenozoic evolution of the region discussed. Within a general framework of convergent plate tectonics, Southeast Asia is also characterized by important extensional tectonics, resulting in the world’s greatest concentration of deep-water marginal basins and Cenozoic sedimentary basins, which have become the focus of the petroleum industry. The pre-Cenozoic geology is too complex for an adequate analysis in this chapter and the reader is referred to Hutchison (1989) for further details. A chronological account summarizing the major geological changes in Southeast Asia is given in Figure 1.2. The main geographical features of the region were established in the Triassic, when the large lithospheric plate of Sinoburmalaya (also known as Sibumasu), which had earlier rifted from the Australian part of Gondwanaland, and collided with and became sutured onto South China and Indochina, together named Cathaysia. The result was a great mountain-building event known as the Indosinian orogeny. Major granites were emplaced during this orogeny, with which the tin and tungsten mineral deposits were genetically related. The orogeny resulted in general uplift and the formation of major new landmasses, which have predominantly persisted as the present-day regional physical geography of Southeast Asia. The Indo-Australian Plate is converging at an average rate of 70 mm a−1 in a 003° direction, pushed from the active South Indian Ocean spreading axis. For the most part it is composed of the Indian Ocean, formed of oceanic sea-floor basalt overlain by deep water. It forms a convergent plate margin with the continental Eurasian Plate, beneath which it subducts at the Sunda or Java Trench. The Eurasian continental plate protrudes as a peninsular extension (Sundaland) southwards as far as Singapore, continuing beneath the shallow Straits of Malacca and the Sunda Shelf as the island of Sumatra and the northwestern part of Borneo.

Treasure maps, sustainable development, and the billion-year stability of cratonic lithosphere

2020 ◽  
Author(s):  
Mark Hoggard ◽  
Karol Czarnota ◽  
Fred Richards ◽  
David Huston ◽  
Lynton Jaques ◽  
...  
Keyword(s):  
Sustainable Development ◽  
Plate Tectonics ◽  
Imaging Techniques ◽  
Mineral Exploration ◽  
Sedimentary Basins ◽  
Clean Energy ◽  
Geological Structure ◽  
Near Surface ◽  
Lithospheric Thickness ◽  
Copper Lead

<p>Sustainable development and transition to a clean-energy economy is placing ever-increasing demand on global supplies of base metals (copper, lead, zinc and nickel). Consumption over the next ~25 years is set to exceed the total produced in human history to date, and it is a growing concern that the rate of exploitation of existing reserves is outstripping discovery of new deposits. Therefore, improvements in the effectiveness of exploration are required to reverse this worrying trend and maintain growth in global living standards.</p><p>Approximately 70% of known lead, 55% of zinc and 20% of copper has been deposited between 2 Ga and recent by low temperature hydrothermal circulation in shallow sedimentary basins. These basins are formed by extension and rifting, which are key manifestations of the plate-mode of tectonics. Despite 150 years of research, the relationship between deposit locations and local geological structure is enigmatic and there remains no accurate technique for predicting their distribution at continental scales.</p><p>Here, we show that modern surface wave tomography and recent parameterisations for anelasticity at seismic frequencies can be used to map lithospheric structure, and that sediment-hosted base metal deposits occur exclusively along the edges of thick lithosphere. Approximately 90% of the world's sediment-hosted copper, lead and zinc resources lie within 200 km of these boundaries, including all giant deposits (>10 megatonnes of metal). Incorporation of higher resolution regional seismic studies into global lithospheric thickness models further enhances the robustness of this relationship. </p><p>This observation implies that lithospheric architecture imparted by the plate-mode of tectonics is stable over billion-year timescales, and that there is a genetic link between lithospheric scale  processes and near-surface hydrothermal mineral systems. Our new maps provide an unprecedented global means to identify fertile regions for targeted mineral exploration, and provide a clear economic justification for funding targeted seismic arrays, theoretical advances in imaging techniques, and geodynamic studies that improve our understanding of deep-time plate tectonics.</p>

Systematics and biogeography of the spider genus Mallinella Strand, 1906, with descriptions of new species and new genera from Southeast Asia (Araneae, Zodariidae)

Zootaxa ◽  
2012 ◽  
Vol 3369 (1) ◽  
pp. 1 ◽  
Author(s):  
PAKAWIN DANKITTIPAKUL ◽  
RUDY JOCQUÉ ◽  
TIPPAWAN SINGTRIPOP
Keyword(s):  
Southeast Asia ◽  
Plate Tectonics ◽  
Indian Subcontinent ◽  
Cladistic Analysis ◽  
Indian Species ◽  
As Species ◽  
History Of ◽  
Nomina Dubia ◽  
Species Groups ◽  
First Time

The systematics status of the spider genus Mallinella Strand, 1906 (Araneae, Zodariidae), the phylogenetic relationshipof the species within the genus and its relationships to other zodariids were investigated by means of cladistic analysis ofmorphological data. Mallinella is redefined and characterized by a single synapomorphy: the presence of posterior ventralspines situated in front of the spinnerets arranged in a single row. The genus is clearly palaeotropical, occurring in Africa,Indian subcontinent, Indo-Burma, Sundaland, Wallacea and Polynesia-Micronesia.Two hundred and two (202) Mallinella species are treated. One hundred and one (101) species are described as newand placed in twenty-two (22) species-groups, making Mallinella the largest zodariid genus. Nineteen (19) species are redescribed, the conspecific sex of seven (7) species is discovered and described for the first time. Fifteen (15) new com-binations are proposed. Nine (9) Storena species are here transferred to Mallinella: M. beauforti (Kulczyński, 1911) comb.nov., M. sciophana (Simon, 1901) comb. nov., M. sobria (Thorell, 1890) comb. nov., M. fasciata (Kulczyński, 1911)comb. nov., M. vicaria (Kulczyński, 1911) comb. nov., M. redimita (Simon, 1905) comb. nov., M. melanognatha (van Has-selt, 1882) comb. nov., M. nilgherina (Simon, 1906) comb. nov., M. vittata (Thorell, 1890) comb. nov. Two Storena spe-cies are transferred to Asceua: A. dispar (Kulczyński, 1911) comb. nov., A. quinquestrigata (Simon, 1905) comb. nov. OneStorena species is transferred to Oedignatha (Liocranidae): O. aleipata (Marples, 1955) comb. nov. One Storena speciesis transferred to Cybaeodamus: C. lentiginosus (Simon, 1905) comb. nov. Storena tricolor Simon, 1908 is transferred tothe Asteron complex of Australia. Three Storena and two Mallinella species are misplaced; they belong to undescribedgenera (S. kraepelini Simon, 1905; S. lesserti Berland, 1938; S. parvula Berland, 1938; M. khanhoa Logunov, 2010; M.rectangulata Zhang et al., 2011). Mallinella vittata (Thorell, 1890) comb. nov. is revalidated and removed from the syn-onymy with M. zebra (Thorell, 1881). Storena vittata Caporiacco, 1955 is removed from homonym replacement (S. ca-poriaccoi Brignoli, 1983) with S. vittata Thorell, 1890 (= M. vittata comb. nov.). Storena annulipes Thorell, 1892 isremoved from its preoccupied name with S. annulipes (L. Koch, 1867) in Storena and transferred to Mallinella; its re-placement name S. cinctipes Simon, 1893 is suppressed.Zodarion luzonicum Simon, 1893, Storena multiguttata Simon, 1893, S. semiflava Simon, 1893 and S. obnubila Si-mon, 1901 are regarded as nomina dubia. Six Indian species were misplaced in Storena; they belong to one of the follow-ing genera: Mallinella, Heliconilla gen. nov., Workmania gen. nov., Heradion, or Euryeidon. These taxa are S. arakuensisPatel & Reddy, 1989, S. debasrae Biswas & Biswas, 1992, S. dibangensis Biswas & Biswas, 2006, S. gujaratensis Tikader& Patel, 1975, S. indica Tikader & Patel, 1975 and S. tikaderi Patel & Reddy, 1989. They are regarded as species incertaesedis.A new genus, Heliconilla gen. nov., is proposed for nine species, six of which are new to science while the otherthree are transferred from Mallinella and Storena. These taxa are: H. irrorata (Thorell, 1887) comb. nov., H. oblonga(Zhang & Zhu, 2009) comb. nov., H. thaleri (Dankittipakul & Schwendinger, 2009) comb. nov.Workmania gen. nov. is established to accommodate two species from Southeast Asia; W. juvenca (Workman, 1896)comb. nov. is transferred from Storena.It is unlikely that the origin of Mallinella dates back more than 100 MYA. Mallinella or its ancestor is believed tohave evolved during the Cretaceous, after the separation of South America from Gondwana, and the greater part of itsevolution took place during the Tertiary. The Asian-Australian lineages of Mallinella could migrate to India via GreaterSomalia before or after the K-T extinction (65 MYA), before the Indian subcontinent joined Asia (ca. 45 MYA).The bio-geographic history of the genus involves plate tectonics during the Cretaceous and the Cenozoic in combination with cli-matic changes and alternating climatic cycles which might have led to episodes of range expansion, isolation of populations and allopatric speciation.

Petrogenesis of Archaean granites in the Barberton region of South Africa as a guide to early crustal evolution

2021 ◽  
Vol 124 (1) ◽  
pp. 111-140
Author(s):  
L.J. Robb ◽  
F.M. Meyer ◽  
C.J. Hawkesworth ◽  
N.J. Gardiner
Keyword(s):  
South Africa ◽  
Continental Crust ◽  
Lower Crust ◽  
Plate Tectonics ◽  
Sedimentary Basins ◽  
Crustal Thickening ◽  
Gravity Inversion ◽  
Crustal Evolution ◽  
Broad Variety ◽  
Parallel Arrays

ABSTRACT The Barberton region of South Africa is characterized by a broad variety of granite types that range in age from ca. 3.5 Ga to 2.7 Ga and reflect the processes involved in the formation of Archaean continental crust on the Kaapvaal Craton. These granites are subdivided into three groups, as follows: A tonalite-trondhjemite-granodiorite (TTG) suite diapirically emplaced at 3 450 Ma and 3 250 Ma into pre-existing metamorphosed greenstone belt material. TTG melts were derived from melting amphibolite in the lower crust, with individual plutons being emplaced at various crustal levels. The dome-and-keel geometry that characterizes the TTG-greenstone dominated crust at this time is inconsistent with a plate tectonic domain and reworking was likely controlled by gravity inversion or ‘sagduction’; Regionally extensive potassic batholiths (the GMS suite) were emplaced at 3 110 Ma during a period of crustal thickening and melting of a TTG-dominated lower crust. Subsequent to emplacement of the voluminous GMS granites, the thickened continental crust had stabilized sufficiently for large sedimentary basins to form; Late granite plutons were emplaced along two distinct linear and sub-parallel arrays close to what might have been the edge of a Kaapvaal continent at 2 800 to 2 700 Ma. They are subdivided into high-Ca and low-Ca granites that resemble the I- and S-type granites of younger orogenic episodes. The high-Ca granites are consistent with derivation from older granitoids in the lower crust, whereas the low-Ca granites may have been derived by melting metasedimentary precursors in the lower-mid crust. Granites with similar characteristics are associated with a subduction zone in younger terranes, although the recognition of such a feature at Barberton remains unclear. The petrogenesis of granites in the Barberton region between 3.5 Ga and 2.7 Ga provides a record of the processes of Archaean crustal evolution and contributes to discussions related to the onset of plate tectonics.

Mesozoic–Tertiary basin models for the Canadian Cordillera and their geological constraints

1977 ◽  
Vol 14 (10) ◽  
pp. 2414-2421 ◽  
Author(s):  
G. H. Eisbacher
Keyword(s):  
Plate Tectonics ◽  
Sedimentary Basins ◽  
Canadian Cordillera ◽  
Reverse Fault ◽  
Late Mesozoic ◽  
Western Cordillera ◽  
Early Tertiary ◽  
Geological Constraints ◽  
Latest Eocene ◽  
Great Valley

Paleogeographic maps for the clastic successions of Early Jurassic, Late Jurassic – Early Cretaceous, and Late Cretaceous – early Tertiary time depict important geologic features that have to be considered in modelling of the Mesozoic sedimentary basins of the Canadian Cordillera. The relative positions of clastic basins, reverse fault zones, and volcanic complexes suggest that the crustal elements underlying the western Cordillera were foreshortened and thickened increasingly from early Mesozoic to early Tertiary. Throughout the late Mesozoic the Canadian Cordillera displayed subdued topography. Uplift was dramatic and possibly of Andean proportions during the latest Eocene and Oligocene. Reconstruction of paleogeography along major right-lateral faults suggests the possibility that old basement trends of the cratonic foreland may have had a profound influence on structures west of the Rocky Mountains. In terms of plate tectonics the Mesozoic basins of the Canadian Cordillera are marginal or possibly intra-arc basins, and cannot be compared easily with the presumed forearc basin containing the late Mesozoic Great Valley Sequence of California.

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