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Text-fig. 2. Distribution of different rock units in the turbidite facies in Majalengka area, West Java, Indonesia. in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 2. Distribution of different rock units in the turbidite facies in Majalengka area, West Java, Indonesia.
Text-fig. 6. Shallowing pattern during the Middle Miocene to Late Miocene/Pliocene due to increasing magmatic activity as an external parameter. a: palaeobathymetry map during the Middle Miocene to Pliocene; b: sea level change curve indicating a shallowing pattern; c: relative changes of sea level and magmatic activity curve (Haq et al. 1987, Soeria-Atmadja et al. 1998, Muljana 2012). in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 6. Shallowing pattern during the Middle Miocene to Late Miocene/Pliocene due to increasing magmatic activity as an external parameter. a: palaeobathymetry map during the Middle Miocene to Pliocene; b: sea level change curve indicating a shallowing pattern; c: relative changes of sea level and magmatic activity curve (Haq et al. 1987, Soeria-Atmadja et al. 1998, Muljana 2012).
Text-fig. 3. Outcrop cross section of the turbidite facies distribution in the Majalengka, correlated northwest to southeast. The progradation pattern indicated by thickening of sandstone into the basin area are shown. F1 – heterolithic sandstone-mudstone 1; F2 – heterolithic sandstone-mudstone 2; F3 – mudstone facies; F4 – heterolithic fine sand and mudstone; F5 – conglomeratic to massive sandstone facies (Muljana 2012). in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 3. Outcrop cross section of the turbidite facies distribution in the Majalengka, correlated northwest to southeast. The progradation pattern indicated by thickening of sandstone into the basin area are shown. F1 – heterolithic sandstone-mudstone 1; F2 – heterolithic sandstone-mudstone 2; F3 – mudstone facies; F4 – heterolithic fine sand and mudstone; F5 – conglomeratic to massive sandstone facies (Muljana 2012).
Text-fig. 4. a: Conglomeratic to massive sandstone facies 1, facies A are composed of Andesit (AF), Clay (CF) and Sandstone (SF) fragments lain on medium-sandstone. b: Conglomeratic to massive sandstone facies, outcropping of massive sandstone facies comprises of fine to medium grain size of grey to yellowish sandstone. c: Heterolithic sandstone-mudstone facies, intercalation of fine sand with silt and shale as type form of heterolithic sandstone mudstone as indicated by a high sand/shale ratio. d: Example outcrops of heterolithic sandstone-mudstone 2 indicated by low sand/shale ratio. e: Heterolithic fine sand and mudstone and mudstone facies, intercalation of thin sandstone and shale. f: Representative of slump deposits outcrops belong to conglomeratic to massive sandstone facies, which is indicated by the intercalation of sandstone and shale and some disturbed beds or layers as seen in slump deposits. The facies type is normally deposited within the basin floor, channel margin or as a product of the overbank deposits. In this figure the slump deposit is shown as internal bedding, some occurred on the bedding-plane. Trend slope measurement of the fold-axis revealed values N 135°E and N 108°E. in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 4. a: Conglomeratic to massive sandstone facies 1, facies A are composed of Andesit (AF), Clay (CF) and Sandstone (SF) fragments lain on medium-sandstone. b: Conglomeratic to massive sandstone facies, outcropping of massive sandstone facies comprises of fine to medium grain size of grey to yellowish sandstone. c: Heterolithic sandstone-mudstone facies, intercalation of fine sand with silt and shale as type form of heterolithic sandstone mudstone as indicated by a high sand/shale ratio. d: Example outcrops of heterolithic sandstone-mudstone 2 indicated by low sand/shale ratio. e: Heterolithic fine sand and mudstone and mudstone facies, intercalation of thin sandstone and shale. f: Representative of slump deposits outcrops belong to conglomeratic to massive sandstone facies, which is indicated by the intercalation of sandstone and shale and some disturbed beds or layers as seen in slump deposits. The facies type is normally deposited within the basin floor, channel margin or as a product of the overbank deposits. In this figure the slump deposit is shown as internal bedding, some occurred on the bedding-plane. Trend slope measurement of the fold-axis revealed values N 135°E and N 108°E.
Text-fig. 5. Several trace fossil types found within turbidite facies in Majalengka area (Muljana 2012). (a) Chondrites, (b) Planolites, (c–e) Thalassinoides, (f) Cruziana?. Scale bar 5 cm. in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 5. Several trace fossil types found within turbidite facies in Majalengka area (Muljana 2012). (a) Chondrites, (b) Planolites, (c–e) Thalassinoides, (f) Cruziana?. Scale bar 5 cm.
Fig. 8 in Macrochelid mites (Acari: Mesostigmata) associated with dung beetles in Mount Gede-Pangrango National Park, West Java, Indonesia
Fig. 8. Sternal shield of A. Macrocheles gedeensis with l.o.p. connected to l.m.t. and B. of M. persimilis which is disjunct to l.m.t.
Fig. 1 in Butterfly (Lepidoptera: Rhopalocera) Distribution Along An Altitudinal Gradient On Mount Tangkuban Parahu, West Java, Indonesia
Fig. 1. Number of butterfly species at different altitudes along the track from the peak of MTP at Upas Crater (2,080 m a.s.l.) to Situ Lembang (1,600 m a.s.l.). P1 to P11 = plot of samplings.
Fig. 2 in Butterfly (Lepidoptera: Rhopalocera) Distribution Along An Altitudinal Gradient On Mount Tangkuban Parahu, West Java, Indonesia
Fig. 2. Frequency of butterfly occurrence along the observation track from Upas Crater to Situ Lembang at MTP during October 2002. 1 = Mycalesis sudra; 2 = Ypthima pandocus; 3 = Pyrameis dejeani; 4 = Faunis canens; 5 = Danaus melaneus; 6 = Pantoporia selenophora; 7 = Neptis mahendra; 8 = Celastrina ceyx; 9 = Cynthia cardui; 10 = Papilio memnon; 11 = Symbrenthia hyplesis; 12 = Celastrina camenae; 13 = Potanthus omaha; 14 = Graphium sarpedon; 15 = Eurema andersonii; 16 = Heliophorus moorei; 17 = Zemeros flegyas; 18 = Chilades pandava; 19 = Jamides abdul; 20 = Abisara savitri; 21 = Lampides boeticus; 22 = Leptosia nina malayana; 23 = Kaniska canace perakana
Fig. 8 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 8. Distributions map of S. testudinaria and S. kawaluensis new species in Java: S. testudinaria is indicated by black spot, S. kawaluensis new species is indicated by star.
Fig. 4 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 4. Radular morphology: A–B, SEM images of a radular fragment of S. kawaluensis new species, showing central, lateral, marginal teeth: A, view from above; B, anterior viewed at 45° showing the shape of radular denticles. C–D, SEM images of radular fragment of S. testudinaria showing central, lateral, marginal teeth: C, view from above; D, anterior viewed at 45° showing the shape of radular denticles. Scale bar = 100 μm.
Fig. 7 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 7. Comparison of shells by parameters of length and shell width of S. kawaluensis new species (n = 36) and S.testudinaria (n = 18), both species from Cibangbay river.
Fig. 6 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 6. Embryonic shells from brood pouches: A, B, S. kawaluensis new species; C, D, S. testudinaria. Scale bar = 0.5 mm.
Fig. 3 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 3. External and internal morphology of S. kawaluensis new species: A, coiling animal; B, detail stomach. Abbreviations: cr, crescent folds; ct, crescent thickenings;dg, digestive gland; dgd, digestive gland duct; gp, gastric pad; lf, lateral fold; me, mantle edge; msc, columella muscle; sa, sorting area; sl, sole; ss, opening to style sac; stm, stomach. Scale bar = 1 mm.
Fig. 1 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 1. Shell morphology of Sulcospira sulcospira, S. pisum, and S. testudinaria: A, holotype S. sulcospira (ZMZ 522306); B, lectotype of Melania pisum MHNG, Brot collection (Java); C, paralectotype of M. pisum, MHNG, Brot collection (Java); D–F, S. testudinaria: (D, MZB Gst.15.062; E, MZB.Gst.15.479; F, MZB Gst.15.481). Abbreviations: ZMZ, Zoologiches Museum der Universität Zürich; MHNG, Muséum d'Histoire Naturelle, Genève. Scale bar = 10 mm.
Fig. 2 in The Freshwater Snail Genus Sulcospira Troschel, 1857 From Java, With Description Of A New Species From Tasikmalaya, West Java, Indonesia (Mollusca: Gastropoda: Pachychilidae)
Fig. 2. Shell and operculum of S. kawaluensis new species: A–C, holotype (MZB Gst.15.059); D, operculum of a paratype; E–G, paratypes (MZB Gst.8.545). Scale bar = 10 mm.
Aftershock Relocation of the November 21, 2022 Cianjur (West Java - Indonesia) Earthquake using Temporary Seismic Network
<p>Aftershock Relocation of the November 21, 2022 Cianjur (West Java - Indonesia) Earthquake using Temporary Seismic Network </p>
Text-fig. 1. Location of study area within Majalengka, West Java, Indonesia. in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
Text-fig. 1. Location of study area within Majalengka, West Java, Indonesia.
Subspecies and Distribution. R. a. afinis Horsfield, 1823 - Malay Peninsula (including Langkawi and Tioman Is), Sumatra, North Pagai I in Mentawai Is, and Java. R. a. hainanusJ. A. Allen, 1906 - Hainan I, China. R. a. himalayanus K Andersen, 1905 — N India (Uttarakhand, Uttar Pradesh, Sikkim, West Bengal, Assam, Meghalaya, Arunachal Pradesh, and Nagaland), Nepal, Bhutan, NE Bangladesh, N Myanmar, and C & S China (Sichuan, Yunnan, Shaanxi, Hubei, Hunan, and Guizhou). R. a. macrurus K. Andersen, 1905 - SE China (Jiangsu, Anhui, Zhejiang, Jiangxi, Fujian, Guangdong, Hong Kong, and Guangxi), S Myanmar, Thailand, Laos, and Vietnam (including Dao Tra Ban and Phu Quoc Is); possibly also Cambodia. R. a. nesites K. Andersen, 1905 - Borneo (including Laut, Sebuku, and Laut Kecil Is) and Anamba and Natuna Is. R. a. princeps K. Andersen, 1905 — Kangean (Kangean and Sepanjang Is), Lombok, Sumbawa, Flores, and Sumba Is. A morphologically distinct subspecies (still unnamed) is known from E Myanmar and N Vietnam. in Rhinolophidae
Subspecies and Distribution. R. a. afinis Horsfield, 1823 - Malay Peninsula (including Langkawi and Tioman Is), Sumatra, North Pagai I in Mentawai Is, and Java. R. a. hainanusJ. A. Allen, 1906 - Hainan I, China. R. a. himalayanus K Andersen, 1905 — N India (Uttarakhand, Uttar Pradesh, Sikkim, West Bengal, Assam, Meghalaya, Arunachal Pradesh, and Nagaland), Nepal, Bhutan, NE Bangladesh, N Myanmar, and C & S China (Sichuan, Yunnan, Shaanxi, Hubei, Hunan, and Guizhou). R. a. macrurus K. Andersen, 1905 - SE China (Jiangsu, Anhui, Zhejiang, Jiangxi, Fujian, Guangdong, Hong Kong, and Guangxi), S Myanmar, Thailand, Laos, and Vietnam (including Dao Tra Ban and Phu Quoc Is); possibly also Cambodia. R. a. nesites K. Andersen, 1905 - Borneo (including Laut, Sebuku, and Laut Kecil Is) and Anamba and Natuna Is. R. a. princeps K. Andersen, 1905 — Kangean (Kangean and Sepanjang Is), Lombok, Sumbawa, Flores, and Sumba Is. A morphologically distinct subspecies (still unnamed) is known from E Myanmar and N Vietnam.
Subspecies and Distribution. R.p. pusillus Temminck, 1834 - N Sumatra, N, E & S Borneo (including Banggi I), W Java, and Bali I. R. p. blythi K. Andersen, 1918 - N India (Uttarakhand, Sikkim, West Bengal, Assam, Meghalaya, and Arunachal Pradesh), Nepal, Bhutan, and SE Bangladesh. R.p. calidusG. M. Allen, 1923-SE China (Guizhou, Guangxi, Guangdong, and Fujian, along with a recent record from Beijing area that may represent this subspecies). R. p. gracilis K. Andersen, 1905 - S India (Andhra Pradesh, Karnataka, Kerala, and Tamil Nadu). R.p. lakkhanae Yoshiyuki, 1990 - S China (Yunnan), Thailand, Laos, Vietnam (including Cat Ba I), Cambodia, and Peninsular Malaysia (including Tioman I). R.p. minutillusG. S. Miller, 1906 —Anambas Is (Siantan). R.p. pagi Tate & Archbold, 1939 — Mentawai Is (North Pagai). R.p. parcus G. M. Allen, 1928 - Hainan I, China. R. p. szechwanus K Andersen, 1918 - Myanmar and C China (Sichuan, Guizhou, Hubei, and probably Yunnan). in Rhinolophidae
Subspecies and Distribution. R.p. pusillus Temminck, 1834 - N Sumatra, N, E & S Borneo (including Banggi I), W Java, and Bali I. R. p. blythi K. Andersen, 1918 - N India (Uttarakhand, Sikkim, West Bengal, Assam, Meghalaya, and Arunachal Pradesh), Nepal, Bhutan, and SE Bangladesh. R.p. calidusG. M. Allen, 1923-SE China (Guizhou, Guangxi, Guangdong, and Fujian, along with a recent record from Beijing area that may represent this subspecies). R. p. gracilis K. Andersen, 1905 - S India (Andhra Pradesh, Karnataka, Kerala, and Tamil Nadu). R.p. lakkhanae Yoshiyuki, 1990 - S China (Yunnan), Thailand, Laos, Vietnam (including Cat Ba I), Cambodia, and Peninsular Malaysia (including Tioman I). R.p. minutillusG. S. Miller, 1906 —Anambas Is (Siantan). R.p. pagi Tate & Archbold, 1939 — Mentawai Is (North Pagai). R.p. parcus G. M. Allen, 1928 - Hainan I, China. R. p. szechwanus K Andersen, 1918 - Myanmar and C China (Sichuan, Guizhou, Hubei, and probably Yunnan).
Relocated Earthquake Catalog (Shallow Depth) for West Java-Indonesia (2009 to 2015)
<p>Relocated Earthquake Catalog (Shalloh Depth) for West Java-Indonesia (2009 to 2015)</p> <p>Please refer to:</p> <p>Supendi, P., Nugraha, A.D., Puspito, N.T., Widiyantoro, S., Daryono, D. (2018). Identification of active faults in West Java, Indonesia, based on earthquake hypocenter determination, relocation, and focal mechanism analysis. Geosci. Lett. 5, 31, https://doi.org/10.1186/s40562-018-0130-y</p>
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