Cekungan Kutai: Perbedaan antara revisi
Konten dihapus Konten ditambahkan
←Membuat halaman berisi 'thumb|Letak Pulau Kalimantan Berkas:Borneo Topography Kutai basin.png|thumb|Topografi Borneo. Cekungan Kutai digambarkan dalam warna bi...' |
rev |
||
| Baris 2: | Baris 2: | ||
[[Berkas:Borneo Topography Kutai basin.png|thumb|Topografi Borneo. Cekungan Kutai digambarkan dalam warna biru]] |
[[Berkas:Borneo Topography Kutai basin.png|thumb|Topografi Borneo. Cekungan Kutai digambarkan dalam warna biru]] |
||
[[Cekungan sedimen]] Kutai membentang dari dataran tinggi bagian tengah [[Kalimantan]], melintasi pantai timur pulau ini dan menuju [[Selat Makassar]]. With an area of 60,000 km<sup>2</sup>, and depths up to 15 km, the Kutai is the largest and deepest [[Tertiary]] age basin in [[Indonesia]].<ref name="cloke et al 1999" /> [[Plate tectonic]] evolution in the Indonesian region of SE Asia has produced a diverse array of basins in the [[Cenozoic]].<ref name="daly et al 91" /> The Kutai is an extensional basin in a general foreland setting. Its geologic evolution begins in the mid [[Eocene]] and involves phases of extension and [[rifting]], thermal sag, and isostatic subsidence. Rapid, high volume, sedimentation related to uplift and inversion began in the Early Miocene.<ref name="cloke et al 1999" /> The different stages of Kutai basin evolution can be roughly correlated to regional and local tectonic events.<ref name="daly et al 91" /> It is also likely that regional climate, namely the onset of the equatorial ever wet monsoon in early [[Miocene]], has affected the geologic evolution of Borneo and the Kutai basin through the present day.<ref name="hall nichols" /> |
[[Cekungan sedimen]] Kutai membentang dari dataran tinggi bagian tengah [[Kalimantan]], melintasi pantai timur pulau ini dan menuju [[Selat Makassar]]. With an area of 60,000 km<sup>2</sup>, and depths up to 15 km, the Kutai is the largest and deepest [[Tertiary]] age basin in [[Indonesia]].<ref name="cloke et al 1999">{{cite journal|last1=Cloke|first1=I.R.|last2=Moss|first2=S.J.|last3=Craig|first3=J.|title=Structural controls on the evolution of the Kutai Basin, East Kalimantan|journal=Journal of Asian Earth Sciences|date=1 February 1999|volume=17|issue=1|pages=137–156|doi=10.1016/S0743-9547(98)00036-1}}<!--|accessdate=23 February 2015--></ref> [[Plate tectonic]] evolution in the Indonesian region of SE Asia has produced a diverse array of basins in the [[Cenozoic]].<ref name="daly et al 91">{{cite journal|last1=Daly|first1=M.C.|last2=Cooper|first2=M.A.|last3=Wilson|first3=I.|last4=Smith|first4=D.G.|last5=Hooper|first5=B.G.D.|title=Cenozoic plate tectonics and basin evolution in Indonesia|url=http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.491.9017&rep=rep1&type=pdf|journal=[[Marine and Petroleum Geology]]|date=February 1991|volume=8|pages=2–20|accessdate=23 February 2015|doi=10.1016/0264-8172(91)90041-x}}</ref> The Kutai is an extensional basin in a general foreland setting. Its geologic evolution begins in the mid [[Eocene]] and involves phases of extension and [[rifting]], thermal sag, and isostatic subsidence. Rapid, high volume, sedimentation related to uplift and inversion began in the Early Miocene.<ref name="cloke et al 1999" /> The different stages of Kutai basin evolution can be roughly correlated to regional and local tectonic events.<ref name="daly et al 91" /> It is also likely that regional climate, namely the onset of the equatorial ever wet monsoon in early [[Miocene]], has affected the geologic evolution of Borneo and the Kutai basin through the present day.<ref name="hall nichols" /> |
||
== Lihat juga == |
== Lihat juga == |
||
Revisi per 1 Oktober 2018 11.07
Cekungan sedimen Kutai membentang dari dataran tinggi bagian tengah Kalimantan, melintasi pantai timur pulau ini dan menuju Selat Makassar. With an area of 60,000 km2, and depths up to 15 km, the Kutai is the largest and deepest Tertiary age basin in Indonesia.[1] Plate tectonic evolution in the Indonesian region of SE Asia has produced a diverse array of basins in the Cenozoic.[2] The Kutai is an extensional basin in a general foreland setting. Its geologic evolution begins in the mid Eocene and involves phases of extension and rifting, thermal sag, and isostatic subsidence. Rapid, high volume, sedimentation related to uplift and inversion began in the Early Miocene.[1] The different stages of Kutai basin evolution can be roughly correlated to regional and local tectonic events.[2] It is also likely that regional climate, namely the onset of the equatorial ever wet monsoon in early Miocene, has affected the geologic evolution of Borneo and the Kutai basin through the present day.[3]
Lihat juga
Referensi
- ^ a b Cloke, I.R.; Moss, S.J.; Craig, J. (1 February 1999). "Structural controls on the evolution of the Kutai Basin, East Kalimantan". Journal of Asian Earth Sciences. 17 (1): 137–156. doi:10.1016/S0743-9547(98)00036-1.
- ^ a b Daly, M.C.; Cooper, M.A.; Wilson, I.; Smith, D.G.; Hooper, B.G.D. (February 1991). "Cenozoic plate tectonics and basin evolution in Indonesia". Marine and Petroleum Geology. 8: 2–20. doi:10.1016/0264-8172(91)90041-x. Diakses tanggal 23 February 2015.
- ^ Kesalahan pengutipan: Tag
<ref>tidak sah; tidak ditemukan teks untuk ref bernamahall nichols